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  <front>
    <journal-meta><journal-id journal-id-type="publisher">ACP</journal-id><journal-title-group>
    <journal-title>Atmospheric Chemistry and Physics</journal-title>
    <abbrev-journal-title abbrev-type="publisher">ACP</abbrev-journal-title><abbrev-journal-title abbrev-type="nlm-ta">Atmos. Chem. Phys.</abbrev-journal-title>
  </journal-title-group><issn pub-type="epub">1680-7324</issn><publisher>
    <publisher-name>Copernicus Publications</publisher-name>
    <publisher-loc>Göttingen, Germany</publisher-loc>
  </publisher></journal-meta>
    <article-meta>
      <article-id pub-id-type="doi">10.5194/acp-18-3433-2018</article-id><title-group><article-title>Comparison and evaluation of anthropogenic emissions<?xmltex \hack{\break}?> of
<inline-formula><mml:math id="M1" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> and <inline-formula><mml:math id="M2" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> over China</article-title>
      </title-group><?xmltex \runningtitle{Comparison and evaluation of anthropogenic emissions of
{$\chem{SO_{2}}$} and $\text{NO}_{{x}}$ over China}?><?xmltex \runningauthor{M.~Li et~al.}?>
      <contrib-group>
        <contrib contrib-type="author" corresp="yes" rid="aff1 aff3 aff5">
          <name><surname>Li</surname><given-names>Meng</given-names></name>
          <email>m.li@mpic.de</email>
        <ext-link>https://orcid.org/0000-0001-5418-9177</ext-link></contrib>
        <contrib contrib-type="author" corresp="no" rid="aff2">
          <name><surname>Klimont</surname><given-names>Zbigniew</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff1">
          <name><surname>Zhang</surname><given-names>Qiang</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff4">
          <name><surname>Martin</surname><given-names>Randall V.</given-names></name>
          
        <ext-link>https://orcid.org/0000-0003-2632-8402</ext-link></contrib>
        <contrib contrib-type="author" corresp="yes" rid="aff3">
          <name><surname>Zheng</surname><given-names>Bo</given-names></name>
          <email>bo.zheng@lsce.ipsl.fr</email>
        <ext-link>https://orcid.org/0000-0001-8344-3445</ext-link></contrib>
        <contrib contrib-type="author" corresp="no" rid="aff2">
          <name><surname>Heyes</surname><given-names>Chris</given-names></name>
          
        <ext-link>https://orcid.org/0000-0001-5254-493X</ext-link></contrib>
        <contrib contrib-type="author" corresp="no" rid="aff2">
          <name><surname>Cofala</surname><given-names>Janusz</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff1 aff5">
          <name><surname>Zhang</surname><given-names>Yuxuan</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff3">
          <name><surname>He</surname><given-names>Kebin</given-names></name>
          
        </contrib>
        <aff id="aff1"><label>1</label><institution>Ministry of Education Key Laboratory for Earth System
Modeling, Department for Earth System Science,<?xmltex \hack{\break}?> Tsinghua University,
Beijing, China</institution>
        </aff>
        <aff id="aff2"><label>2</label><institution>International Institute for Applied Systems Analysis
(IIASA), Laxenburg, 2361, Austria</institution>
        </aff>
        <aff id="aff3"><label>3</label><institution>State Key Joint Laboratory of Environment Simulation and
Pollution Control, School of Environment,<?xmltex \hack{\break}?> Tsinghua University,
Beijing, China</institution>
        </aff>
        <aff id="aff4"><label>4</label><institution>Department of Physics and Atmospheric Science, Dalhousie
University, Halifax, Canada</institution>
        </aff>
        <aff id="aff5"><label>a</label><institution>now at: Max-Planck Institute for Chemistry, Mainz, Germany</institution>
        </aff>
      </contrib-group>
      <author-notes><corresp id="corr1">Meng Li (m.li@mpic.de) and Bo Zheng (bo.zheng@lsce.ipsl.fr)</corresp></author-notes><pub-date><day>8</day><month>March</month><year>2018</year></pub-date>
      
      <volume>18</volume>
      <issue>5</issue>
      <fpage>3433</fpage><lpage>3456</lpage>
      <history>
        <date date-type="received"><day>9</day><month>July</month><year>2017</year></date>
           <date date-type="accepted"><day>6</day><month>February</month><year>2018</year></date>
           <date date-type="rev-recd"><day>22</day><month>January</month><year>2018</year></date>
           <date date-type="rev-request"><day>4</day><month>August</month><year>2017</year></date>
      </history>
      <permissions>
        
        
      <license license-type="open-access"><license-p>This work is licensed under the Creative Commons Attribution 4.0 International License. To view a copy of this licence, visit <ext-link ext-link-type="uri" xlink:href="https://creativecommons.org/licenses/by/4.0/">https://creativecommons.org/licenses/by/4.0/</ext-link></license-p></license></permissions><self-uri xlink:href="https://acp.copernicus.org/articles/.html">This article is available from https://acp.copernicus.org/articles/.html</self-uri><self-uri xlink:href="https://acp.copernicus.org/articles/.pdf">The full text article is available as a PDF file from https://acp.copernicus.org/articles/.pdf</self-uri>
      <abstract>
    <p id="d1e209">Bottom-up emission inventories provide primary understanding of
sources of air pollution and essential input of chemical transport
models. Focusing on <inline-formula><mml:math id="M3" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> and <inline-formula><mml:math id="M4" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>, we conducted
a comprehensive evaluation of two widely used anthropogenic emission
inventories over China, ECLIPSE and MIX, to explore the potential
sources of uncertainties and find clues to improve emission
inventories. We first compared the activity rates and emission
factors used in two inventories and investigated the reasons of
differences and the impacts on emission estimates. We found that
<inline-formula><mml:math id="M5" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> emission estimates are consistent between two
inventories (with 1 % differences), while <inline-formula><mml:math id="M6" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>
emissions in ECLIPSE's estimates are 16 % lower than those of
MIX. The FGD (flue-gas desulfurization) device penetration rate and
removal efficiency, LNB (low-<inline-formula><mml:math id="M7" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> burner) application
rate and abatement efficiency in power plants, emission factors of
industrial boilers and various vehicle types, and vehicle fleet need
further verification. Diesel consumptions are quite uncertain in
current inventories. Discrepancies at the sectorial and provincial levels
are much higher than those of the national total. We then examined
the impacts of different inventories on model performance by using
the nested GEOS-Chem model. We finally derived top-down emissions by
using the retrieved columns from the Ozone Monitoring Instrument
(OMI) compared with the bottom-up estimates. High correlations
were observed for <inline-formula><mml:math id="M8" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> between model results and OMI
columns. For <inline-formula><mml:math id="M9" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>, negative biases in bottom-up gridded
emission inventories (<inline-formula><mml:math id="M10" display="inline"><mml:mo>-</mml:mo></mml:math></inline-formula>21 % for MIX, <inline-formula><mml:math id="M11" display="inline"><mml:mo>-</mml:mo></mml:math></inline-formula>39 % for ECLIPSE)
were found compared to the satellite-based emissions. The emission trends
from 2005 to 2010 estimated by two inventories were both consistent
with satellite observations. The inventories appear to be fit for evaluation of
the policies at an aggregated or national level; more work is needed
in specific areas in order to improve the accuracy and robustness of
outcomes at finer spatial and also technological levels. To our
knowledge, this is the first work in which source comparisons
detailed to technology-level parameters are made along with the
remote sensing retrievals and chemical transport modeling.  Through
the comparison between bottom-up emission inventories and evaluation
with top-down information, we identified potential directions for
further improvement in inventory development.</p>
  </abstract>
    </article-meta>
  </front>
<body>
      

<sec id="Ch1.S1" sec-type="intro">
  <title>Introduction</title>
      <p id="d1e311"><inline-formula><mml:math id="M12" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> and <inline-formula><mml:math id="M13" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> are important precursors of secondary
<inline-formula><mml:math id="M14" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">PM</mml:mi><mml:mn mathvariant="normal">2.5</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>, contributing to severe environmental problems
including haze and acid rain, and have been shown to be detrimental to human
health and ecosystems (Seinfeld and Pandis, 2006). China's
anthropogenic emissions have become one of the major contributors to
the global budget during the last decade (Klimont et al., 2013; Hoesly
et al., 2018). To support chemical transport modeling and provide
scientific basis for policy-making, several emission inventories
covering China have been developed (Streets et al., 2003; Ohara
et al., 2007; Zhang et al., 2007, 2009; Lu et al., 2010, 2011;
Kurokawa et al., 2013; Klimont et al., 2009, 2013; Wang et al., 2014;
Li et al., 2017; EDGAR v4.2, available at
<uri>http://edgar.jrc.ec.europa.eu</uri>).</p>
      <p id="d1e349">Bottom-up emissions are estimated through comprehensive
parameterization of fuel consumption, industrial production, emission
factors and mitigation measures and spatially allocated to satisfy
the chemical and climate model requirements. Uncertainties of
emissions have been qualitatively illustrated (e.g., Granier et al.,
2011; Saikawa et al., 2017) or quantitatively analyzed (Streets
et al., 2003; Zhao et al., 2011; Guan et al., 2012; Hong et al.,
2017), inferring significant gaps in activity statistics and control
measures' assumptions in emission inventories developed for different
spatial scales (i.e., global, regional, or city scale; Zhao et al.,
2015).</p>
      <p id="d1e352">Extensive comparisons of emission inventories have been conducted to
illustrate the impacts of variable emissions on the model simulation
results (e.g., Saikawa et al., 2017; Zhou et al., 2017). Although they
provide important indications on the extent of discrepancies, there
are still gaps for applying the comparison results to improve the
inventory accuracy:
<list list-type="order"><list-item><p id="d1e356">Comparisons have been conducted for the total anthropogenic
sources, instead of by sectors, subsectors, and sources. Inconsistency of
source categories included in inventory models were not overviewed
or analyzed.</p></list-item><list-item><p id="d1e359">Few studies go into the comparisons on a specific parameter level
because the technology-based framework for each inventory was not
publicly available.</p></list-item><list-item><p id="d1e362">Top-down and bottom-up comparisons have not been comprehensively
combined to infer the potential uncertain parameters for all key
sectors.</p></list-item></list></p>
      <p id="d1e365">To further improve the accuracy of emission estimation, we compared and
evaluated the global ECLIPSE (Evaluating the Climate and Air Quality Impacts
of Short-Lived Pollutants; Klimont et al., 2017) and MIX Asian (Li et al.,
2017) inventories due to the following reasons: (a) Up to the time of paper
preparation, ECLIPSE and MIX were the only publicly accessible gridded
emission datasets that include both <inline-formula><mml:math id="M15" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> and <inline-formula><mml:math id="M16" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> covering
China for the period of 2005 and 2010; (b) both inventories have been widely
applied in atmospheric modeling and policy discussions (e.g., Stohl et al.,
2015; Duan et al., 2016; Galmarini et al., 2017; Rao et al., 2017); (c) the
technology-based framework and compiling parameters by source categories are
obtained for ECLIPSE and MIX through international collaboration, which is
not accessible for other inventories over China. The methods and data were
extensively described by a series of papers (Zheng et al., 2014; Liu et al.,
2015; Klimont et al., 2017; Li et al., 2017), supporting us for explicit
comparisons and analyses; (d) ECLIPSE (GAINS model, Greenhouse gas-Air
pollution Interactions and Synergies model; Amann et al., 2011) can be
representative of the state-of-science global emission inventory covering
China, and MIX (MEIC model, Multi-resolution Emission Inventory for China;
available at <uri>www.meicmodel.org</uri>) represents the regional inventory
compiled with advanced methods and local data. The methods, parameters and
assumptions of GAINS and MEIC are always referred to by inventory developers
(e.g., Lu et al., 2010; Fu et al., 2013; Kurokawa et al., 2013; Zhao et al.,
2013). The comparisons and validations are important to improve the accuracy
of gridded emissions and model performance over China.</p>
      <p id="d1e394">Another motivation of this work is to discuss the “fitness” of current
developed inventories (specifically ECLIPSE and MIX) and modeling work
performed with them for policy-relevant discussion. The inventories and the
relevant modeling work are playing an increasingly important role for policy
discussion in Europe and most recently more and more in Asia on different
scales. However, there are no systematic and officially approved methods and
inventories but a variety of scientific products. While a lot of effort has
been made to validate emission estimates with measurements, higher source and
spatial resolution of inventories and projections will also serve discussion
about how to shape future policies to reduce impact of air pollution. In this
work, we compared the ECLIPSE and MIX emissions over China at a detailed
activity-source level. What we focused on in this paper is the bottom-up
comparison detailed to a specific parameter contributing to the differences
between the two widely used gridded emission inventories (ECLIPSE and MIX),
combined with top-down validations from the satellite observations. We
compared the activity rates and emission factors derived from several key
parameters for the largest sources for each sector and subsector.
Discrepancies in the methodologies used, data sources, technology penetration
assumptions and spatial emission patterns are discussed and illustrated.
Furthermore, we combined the bottom-up comparisons with top-down evaluations
based on observations of the OMI (Ozone Monitoring Instrument) aboard the
Aura satellite
(Levelt et al., 2006). To our knowledge, this is the first emission inventory
assessment work in which parameter-level comparison and remote sensing
evaluations are combined. OMI data provide essential constraints on emission
estimates, spatial distributions and trends (Wang et al., 2012; Liu et al.,
2016). In recent work described by Geng et al. (2017), OMI <inline-formula><mml:math id="M17" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">NO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>
columns were applied to analyze and evaluate the sensitivities of spatial
proxies used in the emission gridding process.</p>
      <p id="d1e408">Methodology and data used are summarized in Sect. 2. Bottom-up
comparisons of emissions are illustrated by decomposing the elements
of inventory development in Sect. 3.1. Section 3.2 presents the
evaluations and constraints from a satellite perspective. A summary of key
reasons leading to emission discrepancies is provided in
Sect. 3.3. Finally, Sect. 4 gives the concluding remarks.</p>
</sec>
<sec id="Ch1.S2">
  <title>Methodology and data</title>
<sec id="Ch1.S2.SS1">
  <title>The ECLIPSE and MIX emission inventory</title>
      <p id="d1e422">Spatially specific emission inventories of air pollutants and
greenhouse gases are among key inputs for chemical transport models
(CTMs) and climate models. ECLIPSE (Klimont et al., 2017) and MIX (Li
et al., 2017) emission inventories have been applied in numerous
modeling activities at global (Stohl et al., 2015) and regional
levels, within the ECLIPSE and MICS-Asia (Model Intercomparison Study
for Asia) Phase III projects, respectively. In general, both
inventories use a dynamic technology-based methodology to estimate
anthropogenic emissions by multiplying activity rates with
technology-specific emission factors for each source by administrative
unit (province or county) (Klimont et al., 2017; Li et al., 2017). Then,
spatial proxies are used to distribute emission estimates by
province or county to grids to satisfy the needs of model simulation. The
key features of both inventories are listed in Table 1.</p>

<?xmltex \floatpos{t}?><table-wrap id="Ch1.T1" specific-use="star"><caption><p id="d1e428">Key features of ECLIPSE v5a and MIX emission inventories.</p></caption><oasis:table frame="topbot"><oasis:tgroup cols="3">
     <oasis:colspec colnum="1" colname="col1" align="left"/>
     <oasis:colspec colnum="2" colname="col2" align="justify" colwidth="150pt"/>
     <oasis:colspec colnum="3" colname="col3" align="justify" colwidth="160pt"/>
     <oasis:thead>
       <oasis:row rowsep="1">  
         <oasis:entry colname="col1">Item</oasis:entry>  
         <oasis:entry colname="col2">ECLIPSE v5a</oasis:entry>  
         <oasis:entry colname="col3">MIX</oasis:entry>
       </oasis:row>
     </oasis:thead>
     <oasis:tbody>
       <oasis:row>  
         <oasis:entry colname="col1">Year</oasis:entry>  
         <oasis:entry colname="col2">1990–2010 at 5-year intervals</oasis:entry>  
         <oasis:entry colname="col3">2005<inline-formula><mml:math id="M22" display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">a</mml:mi></mml:msup></mml:math></inline-formula>, 2008, 2010</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1">Domain</oasis:entry>  
         <oasis:entry colname="col2">Global</oasis:entry>  
         <oasis:entry colname="col3">Asia</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1">Spatial resolution</oasis:entry>  
         <oasis:entry colname="col2"><inline-formula><mml:math id="M23" display="inline"><mml:mrow><mml:mn mathvariant="normal">0.5</mml:mn><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup><mml:mo>×</mml:mo><mml:mn mathvariant="normal">0.5</mml:mn><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:mrow></mml:math></inline-formula></oasis:entry>  
         <oasis:entry colname="col3"><inline-formula><mml:math id="M24" display="inline"><mml:mrow><mml:mn mathvariant="normal">0.25</mml:mn><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup><mml:mo>×</mml:mo><mml:mn mathvariant="normal">0.25</mml:mn><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:mrow></mml:math></inline-formula></oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">  
         <oasis:entry colname="col1">Temporal resolution</oasis:entry>  
         <oasis:entry colname="col2">Monthly</oasis:entry>  
         <oasis:entry colname="col3">Monthly</oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">  
         <oasis:entry namest="col1" nameend="col3">Activities included for each sector </oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1">Energy/power</oasis:entry>  
         <oasis:entry colname="col2">Power plants (including combined heat and power), energy<?xmltex \hack{\hfill\break}?>production–conversion (including district heating plants), fossil fuel distribution</oasis:entry>  
         <oasis:entry colname="col3">Power plants (including combined heat and power)</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1">Industry</oasis:entry>  
         <oasis:entry colname="col2">Industrial combustion and processes</oasis:entry>  
         <oasis:entry colname="col3">Industrial combustion (including industrial<?xmltex \hack{\hfill\break}?>heating plants) and industrial processes</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1">Residential</oasis:entry>  
         <oasis:entry colname="col2">Residential combustion sources</oasis:entry>  
         <oasis:entry colname="col3">Residential combustion sources (including<?xmltex \hack{\hfill\break}?>residential heating plants)</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1">Transportation</oasis:entry>  
         <oasis:entry colname="col2">On-road and off-road transport sources<inline-formula><mml:math id="M25" display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">b</mml:mi></mml:msup></mml:math></inline-formula></oasis:entry>  
         <oasis:entry colname="col3">On-road and off-road transport sources<inline-formula><mml:math id="M26" display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">b</mml:mi></mml:msup></mml:math></inline-formula></oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">  
         <oasis:entry colname="col1">Agriculture</oasis:entry>  
         <oasis:entry colname="col2">Livestock and fertilization</oasis:entry>  
         <oasis:entry colname="col3">Livestock and fertilization</oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">  
         <oasis:entry namest="col1" nameend="col3">Data sources of activity rates </oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1">Power</oasis:entry>  
         <oasis:entry colname="col2">International Energy Agency (IEA)</oasis:entry>  
         <oasis:entry colname="col3">CPED (Liu et al., 2015)</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1">Industry</oasis:entry>  
         <oasis:entry colname="col2">International Energy Agency (IEA)</oasis:entry>  
         <oasis:entry colname="col3">Provincial industrial economy<?xmltex \hack{\hfill\break}?>statistics (NBS)</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1">Residential</oasis:entry>  
         <oasis:entry colname="col2">International Energy Agency (IEA)</oasis:entry>  
         <oasis:entry colname="col3">Provincial energy statistics (NBS)</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1">Transportation</oasis:entry>  
         <oasis:entry colname="col2">International Energy Agency (IEA)</oasis:entry>  
         <oasis:entry colname="col3">Provincial energy statistics (NBS);<?xmltex \hack{\hfill\break}?>Zheng et al. (2014)</oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">  
         <oasis:entry colname="col1">Agriculture</oasis:entry>  
         <oasis:entry colname="col2">UN Food and Agriculture Organization<inline-formula><mml:math id="M27" display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">c</mml:mi></mml:msup></mml:math></inline-formula></oasis:entry>  
         <oasis:entry colname="col3">Provincial statistics (NBS,<?xmltex \hack{\hfill\break}?>Huang et al., 2012)</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1">Emission factors and technology</oasis:entry>  
         <oasis:entry colname="col2">GAINS model (Klimont et al., 2017)</oasis:entry>  
         <oasis:entry colname="col3">MEIC model<inline-formula><mml:math id="M28" display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">d</mml:mi></mml:msup></mml:math></inline-formula>, process-based model for <inline-formula><mml:math id="M29" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">NH</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> (Huang et al., 2012)</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1">Data access</oasis:entry>  
         <oasis:entry colname="col2"><uri>http://www.iiasa.ac.at/web/home/research/researchPrograms/air/ECLIPSEv5a.html</uri></oasis:entry>  
         <oasis:entry colname="col3"><uri>http://www.meicmodel.org/dataset-mix</uri></oasis:entry>
       </oasis:row>
     </oasis:tbody>
   </oasis:tgroup></oasis:table><table-wrap-foot><p id="d1e431"><inline-formula><mml:math id="M18" display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">a</mml:mi></mml:msup></mml:math></inline-formula> Developed following the same methodology of Li et al. (2017).<?xmltex \hack{\\}?><inline-formula><mml:math id="M19" display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">b</mml:mi></mml:msup></mml:math></inline-formula> International air and international shipping are not
included.<?xmltex \hack{\\}?><inline-formula><mml:math id="M20" display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">c</mml:mi></mml:msup></mml:math></inline-formula> FAO, <uri xlink:href="http://www.fao.org/faostat/en/{#}home">http://www.fao.org/faostat/en/#home</uri>.<?xmltex \hack{\\}?><inline-formula><mml:math id="M21" display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">d</mml:mi></mml:msup></mml:math></inline-formula> Zhang et al. (2009);  Lei et al. (2011);  Zheng
et al. (2014);  Liu et al. (2015).</p></table-wrap-foot></table-wrap>

      <p id="d1e815">The ECLIPSE dataset is a global emission inventory for the
period of 1990 to 2010 extended by projections to 2050 in 5-year
intervals with monthly variations, developed with the GAINS model
(Amann et al., 2011).  Primary sources of activity data are the
International Energy Agency (IEA, 2012) for fuel use and the UN Food and
Agriculture Organization for agriculture (FAO,
<uri xlink:href="http://www.fao.org/faostat/en/{#}home">http://www.fao.org/faostat/en/#home</uri>). GAINS distinguishes 172
regions, including provinces for China, for which regionally specific
emission factors and technology distributions are assumed.</p>
      <p id="d1e821">Emissions are distributed to grids at a specific resolution
(<inline-formula><mml:math id="M30" display="inline"><mml:mrow><mml:mn mathvariant="normal">0.5</mml:mn><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup><mml:mo>×</mml:mo><mml:mn mathvariant="normal">0.5</mml:mn><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:mrow></mml:math></inline-formula> for ECLIPSE,
longitude <inline-formula><mml:math id="M31" display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> latitude) based on the percentages of spatial
proxies located in grids by source category using GIS (Geographic
Information System) techniques. For ECLIPSE, several layers were
developed as spatial proxies in line with those used in the
Representative Concentration Pathways (RCP) (Lamarque et al., 2010),
i.e., locations of energy and manufacturing facilities, road networks,
shipping routes, human and animal population density, and agricultural
land use.  Spatial proxies were further developed within the Global
Energy Assessment project (GEA project; Riahi et al., 2012), including
improved population distribution, flaring in oil and gas production,
smelters, and power plants for which provincial emission layers of
MEIC were
used. Spatial proxies for both ECLIPSE and MIX are summarized in
Table S1 in the Supplement.</p>
      <p id="d1e852">In this work, we use a gridded ECLIPSE v5a dataset (current legislation,
CLE;
available at
<uri>http://www.iiasa.ac.at/web/home/research/researchPrograms/air/ECLIPSEv5a.html</uri>)
for 2005 and 2010 in China for all anthropogenic sources excluding
international shipping and aviation to keep source consistency in comparison
to MIX. We developed two sensitivity cases of the ECLIPSE emissions by
changing the emission estimates or spatial proxies to study the effect of
inventory parameterization on model accuracy, as described in Sect. 3.2.1.</p>
      <p id="d1e858">MIX was developed for 2008 and 2010 (including monthly
variation) by combining the up-to-date regional inventories. For
China, the monthly MEIC dataset (available at
<uri>www.meicmodel.org</uri>) and PKU-<inline-formula><mml:math id="M32" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">NH</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> (only for <inline-formula><mml:math id="M33" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">NH</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>)
inventory are used (Li et al., 2017). The MEIC model calculates and
updates emissions for over 700 anthropogenic sources dynamically and
delivers the dataset online. Activity rates are derived from local
provincial statistics in China and emission factors are derived from
the best available local measurements and recent peer-reviewed data
for China. Power plants are treated as point sources with emissions
estimated by fuel type considering actual combustion technology and
installed control measures such as FGD (flue-gas desulfurization); this information is derived from CPED (China coal-fired
Power plant Emissions Database) as described by Liu
et al. (2015). Following the methodology of Zheng et al. (2014),
emissions of the transport sector in MEIC are estimated at the county
level based on comprehensive parameterization of vehicle ownership,
fuel consumption, temporal evolution of emission factors and
implementation of new environmental standards. Volatile organic compounds (VOCs) are speciated to
more than 1000 species and lumped to a GEOS-Chem configured mechanism
based on source-specific composite profiles and mapping tables in Li
et al. (2014).</p>
      <p id="d1e886">Monthly gridded emissions of MEIC are generated by applying
source-based spatial and temporal profiles (Li et al.,
2017). Provincial emissions of MEIC are firstly distributed to counties,
then further distributed to grids.  The former process was based on
statistics by county (i.e., GDP (gross domestic product), industrial
GDP, total population, urban population, rural population,
agricultural activity, vehicle population), and the latter was based
on gridded maps as spatial proxies (i.e., population density map, road
network). For power plants, locations were determined using Google
Earth following the unit-based methodology. Gridded emission products
of MEIC v1.1 at a resolution of <inline-formula><mml:math id="M34" display="inline"><mml:mrow><mml:mn mathvariant="normal">0.25</mml:mn><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup><mml:mo>×</mml:mo><mml:mn mathvariant="normal">0.25</mml:mn><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:mrow></mml:math></inline-formula>
were integrated into MIX. In this work, we updated China's emissions
with MEIC v1.2 and extended the MIX emissions back to 2005 following
the same methodology.</p>
</sec>
<sec id="Ch1.S2.SS2">
  <title>GEOS-Chem</title>
      <p id="d1e915">GEOS-Chem is an open-access global 3-D CTM widely used by about 100
research groups worldwide. The model is driven by the GEOS (Goddard
Earth Observing System) meteorological dataset and includes complete
<inline-formula><mml:math id="M35" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>–<inline-formula><mml:math id="M36" display="inline"><mml:mrow><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>–HC–aerosol chemistry (“full
chemistry”), covering over 80 species and more than 300 chemical
reactions (Bey et al., 2001; Park et al., 2004).</p>
      <p id="d1e940"><?xmltex \hack{\newpage}?>In this work, the Asian-nested grid GEOS-Chem model v9-01-03 driven by GEOS-5
was used to simulate <inline-formula><mml:math id="M37" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> and the <inline-formula><mml:math id="M38" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">NO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>
maps with different emission inventories (Chen et al., 2009). Anthropogenic
emissions for Asia were replaced with MIX and ECLIPSE variants described in
Sect. 3.2.1. The model has a horizontal resolution of <inline-formula><mml:math id="M39" display="inline"><mml:mrow><mml:mn mathvariant="normal">0.667</mml:mn><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup><mml:mo>×</mml:mo><mml:mn mathvariant="normal">0.5</mml:mn><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:mrow></mml:math></inline-formula> (longitude <inline-formula><mml:math id="M40" display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> latitude) covering Asia and 47 vertical
layers. A nonlocal scheme was applied in mixing within the planetary boundary
layer (Lin and McElroy, 2010). Global concentrations at <inline-formula><mml:math id="M41" display="inline"><mml:mrow><mml:mn mathvariant="normal">2.5</mml:mn><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup><mml:mo>×</mml:mo><mml:mn mathvariant="normal">2</mml:mn><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:mrow></mml:math></inline-formula> (longitude <inline-formula><mml:math id="M42" display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> latitude) were simulated to provide
time-varying boundary conditions to the target region. A 1-month spin-up was
conducted to reduce the effect of initial conditions. To compare with the OMI
observations consistently, we averaged the daily modeled vertical columns at
13:00–15:00 local time and resampled the model on grids that have OMI data.</p>
</sec>
<sec id="Ch1.S2.SS3">
  <title>Top-down emission inventory</title>
      <p id="d1e1027">We developed the top-down emission inventories for <inline-formula><mml:math id="M43" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> and
<inline-formula><mml:math id="M44" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> based on the OMI/Aura L2 swath data. For <inline-formula><mml:math id="M45" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>,
we obtained the planetary boundary layer <inline-formula><mml:math id="M46" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> total
vertical columns from GES DISC (Goddard Earth Sciences Data and
Information Services Center) of NASA (Li et al., 2006). The
mass-balance method was used to interpret the top-down anthropogenic
emissions from total columns (Martin et al., 2003; Lee et al.,
2011). For <inline-formula><mml:math id="M47" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>, we used the tropospheric slant <inline-formula><mml:math id="M48" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">NO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>
column data of the DOMINO v2 (Dutch OMI <inline-formula><mml:math id="M49" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">NO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> version 2) product
accessed from the TEMIS website (Tropospheric Emission Monitoring
Internet Service, <uri>http://www.temis.nl/</uri>) (Boersma et al.,
2011). Slant columns were converted to vertical columns using the air
mass factor (AMF), which is sensitive to the <inline-formula><mml:math id="M50" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">NO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> vertical
profile (Palmer et al., 2001; Lamsal et al., 2010). We revised the AMF
by replacing the a priori vertical profiles with the modeled ones to
reduce the bias in comparison following the methodology of Lamsal
et al. (2010). To reduce the retrieval uncertainties, we excluded the
OMI pixels at a solar zenith angle <inline-formula><mml:math id="M51" display="inline"><mml:mrow><mml:mo>≥</mml:mo><mml:mn mathvariant="normal">78</mml:mn></mml:mrow></mml:math></inline-formula><inline-formula><mml:math id="M52" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>, cloud radiance
fraction <inline-formula><mml:math id="M53" display="inline"><mml:mrow><mml:mo>&gt;</mml:mo><mml:mn mathvariant="normal">30</mml:mn></mml:mrow></mml:math></inline-formula> %, surface albedo <inline-formula><mml:math id="M54" display="inline"><mml:mrow><mml:mo>≥</mml:mo><mml:mn mathvariant="normal">0.3</mml:mn></mml:mrow></mml:math></inline-formula> or affected by row
anomaly
(<uri>http://projects.knmi.nl/omi/research/product/rowanomaly-background.php</uri>).
Large pixels near the swath edges (10 pixels on each side) are also
rejected in spatial averaging. Furthermore, daily data of <inline-formula><mml:math id="M55" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>
and <inline-formula><mml:math id="M56" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">NO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> vertical column density were developed after
allocating the OMI pixels to model grids (<inline-formula><mml:math id="M57" display="inline"><mml:mrow><mml:mn mathvariant="normal">0.667</mml:mn><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup><mml:mo>×</mml:mo><mml:mn mathvariant="normal">0.5</mml:mn><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:mrow></mml:math></inline-formula>) based on area weights.</p>
      <p id="d1e1206">Top-down <inline-formula><mml:math id="M58" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> emissions were developed following the finite
difference mass balance (FDMB) methodology (Lamsal et al., 2011;
Cooper et al., 2017).  We used the summer data to develop the top-down
emissions because of the stronger relationship between local emissions
and grid columns. The smearing length is around 50 <inline-formula><mml:math id="M59" display="inline"><mml:mi mathvariant="normal">km</mml:mi></mml:math></inline-formula> over
China in summer (assuming wind speed 5 <inline-formula><mml:math id="M60" display="inline"><mml:mrow><mml:mi mathvariant="normal">m</mml:mi><mml:mspace linebreak="nobreak" width="0.125em"/><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>, <inline-formula><mml:math id="M61" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">NO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>
lifetime 3 <inline-formula><mml:math id="M62" display="inline"><mml:mi mathvariant="normal">h</mml:mi></mml:math></inline-formula>), comparable to the model grid size, implying
weak effects upon the inversion of horizontal mass transport between
grids.  Compared to the basic mass-balance method described in Martin
et al. (2003), the FDMB method reduces the errors from nonlinearity of
<inline-formula><mml:math id="M63" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>–OH–<inline-formula><mml:math id="M64" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> chemistry (Gu et al., 2016; Cooper
et al., 2017). A unitless scaling factor <inline-formula><mml:math id="M65" display="inline"><mml:mi mathvariant="italic">β</mml:mi></mml:math></inline-formula> was introduced to
represent the sensitivity of fractional modeled <inline-formula><mml:math id="M66" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">NO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> columns to
the fractional anthropogenic emission changes for each grid. We
apply 15 % perturbation to emissions, simulate the <inline-formula><mml:math id="M67" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">NO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>
column changes and calculate <inline-formula><mml:math id="M68" display="inline"><mml:mi mathvariant="italic">β</mml:mi></mml:math></inline-formula> following Eq. (<xref ref-type="disp-formula" rid="Ch1.E1"/>)
(Lamsal et al., 2011; Cooper et al., 2017).

                <disp-formula id="Ch1.E1" content-type="numbered"><mml:math id="M69" display="block"><mml:mstyle class="stylechange" displaystyle="true"/><mml:mrow><mml:mstyle displaystyle="true"><mml:mfrac style="display"><mml:mrow><mml:mi mathvariant="normal">Δ</mml:mi><mml:mi>E</mml:mi></mml:mrow><mml:mi>E</mml:mi></mml:mfrac></mml:mstyle><mml:mo>=</mml:mo><mml:mi mathvariant="italic">β</mml:mi><mml:mstyle displaystyle="true"><mml:mfrac style="display"><mml:mrow><mml:mi mathvariant="normal">Δ</mml:mi><mml:mi mathvariant="normal">Ω</mml:mi></mml:mrow><mml:mi mathvariant="normal">Ω</mml:mi></mml:mfrac></mml:mstyle><mml:mo>,</mml:mo></mml:mrow></mml:math></disp-formula>

          where <inline-formula><mml:math id="M70" display="inline"><mml:mi>E</mml:mi></mml:math></inline-formula> represents the total <inline-formula><mml:math id="M71" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> emissions and <inline-formula><mml:math id="M72" display="inline"><mml:mi mathvariant="normal">Ω</mml:mi></mml:math></inline-formula>
represents the local <inline-formula><mml:math id="M73" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">NO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> column. <inline-formula><mml:math id="M74" display="inline"><mml:mrow><mml:mi mathvariant="normal">Δ</mml:mi><mml:mi>E</mml:mi></mml:mrow></mml:math></inline-formula> is the emission
changes of anthropogenic sources, and <inline-formula><mml:math id="M75" display="inline"><mml:mrow><mml:mi mathvariant="normal">Δ</mml:mi><mml:mi mathvariant="normal">Ω</mml:mi></mml:mrow></mml:math></inline-formula> is the column
changes under perturbation.</p>
      <p id="d1e1412">The top-down emissions were further determined based on
Eq. (<xref ref-type="disp-formula" rid="Ch1.E2"/>).

                <disp-formula id="Ch1.E2" content-type="numbered"><mml:math id="M76" display="block"><mml:mstyle displaystyle="true" class="stylechange"/><mml:mrow><mml:mstyle displaystyle="true" class="stylechange"/><mml:msub><mml:mi>E</mml:mi><mml:mi>t</mml:mi></mml:msub><mml:mo>=</mml:mo><mml:msub><mml:mi>E</mml:mi><mml:mi>a</mml:mi></mml:msub><mml:mfenced open="(" close=")"><mml:mn mathvariant="normal">1</mml:mn><mml:mo>+</mml:mo><mml:mstyle displaystyle="true"><mml:mfrac style="display"><mml:mrow><mml:msub><mml:mi mathvariant="normal">Ω</mml:mi><mml:mi>t</mml:mi></mml:msub><mml:mo>-</mml:mo><mml:msub><mml:mi mathvariant="normal">Ω</mml:mi><mml:mi>a</mml:mi></mml:msub></mml:mrow><mml:mrow><mml:msub><mml:mi mathvariant="normal">Ω</mml:mi><mml:mi>a</mml:mi></mml:msub></mml:mrow></mml:mfrac></mml:mstyle><mml:mi mathvariant="italic">β</mml:mi></mml:mfenced><mml:mo>,</mml:mo></mml:mrow></mml:math></disp-formula>

          where <inline-formula><mml:math id="M77" display="inline"><mml:mrow><mml:msub><mml:mi>E</mml:mi><mml:mi>t</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> and <inline-formula><mml:math id="M78" display="inline"><mml:mrow><mml:msub><mml:mi>E</mml:mi><mml:mi>a</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> represent the top-down and priori
emissions, respectively. <inline-formula><mml:math id="M79" display="inline"><mml:mrow><mml:msub><mml:mi mathvariant="normal">Ω</mml:mi><mml:mi>t</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> is the OMI-retrieved
column. <inline-formula><mml:math id="M80" display="inline"><mml:mrow><mml:msub><mml:mi mathvariant="normal">Ω</mml:mi><mml:mi>a</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> is the modeled column of GEOS-Chem.</p>
      <p id="d1e1512">Following Cooper et al. (2017), we limited <inline-formula><mml:math id="M81" display="inline"><mml:mi mathvariant="italic">β</mml:mi></mml:math></inline-formula> within 0.1–10 to
avoid biases in regions with negligible low anthropogenic emissions or
columns.  The absolute error in the retrieved <inline-formula><mml:math id="M82" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">NO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> columns is
estimated at <inline-formula><mml:math id="M83" display="inline"><mml:mrow><mml:mn mathvariant="normal">1</mml:mn><mml:mo>×</mml:mo><mml:msup><mml:mn mathvariant="normal">10</mml:mn><mml:mn mathvariant="normal">15</mml:mn></mml:msup></mml:mrow></mml:math></inline-formula> molecules <inline-formula><mml:math id="M84" display="inline"><mml:mrow><mml:msup><mml:mi mathvariant="normal">cm</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">2</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula> (Martin
et al., 2003). We filtered out the monthly averaged retrieved columns
based on this criterion and further developed the top-down emissions
for each simulation case. Finally, summer-averaged top-down emissions
were developed and applied in the evaluations of this work.</p>
</sec>
</sec>
<sec id="Ch1.S3">
  <title>Results and discussion</title>
<sec id="Ch1.S3.SS1">
  <title>Comparisons of ECLIPSE and MIX</title>
      <p id="d1e1574">Following the framework of gridded emission inventory development, we
conducted parameter-level comparisons between ECLIPSE and MIX and
quantified the reasons causing the emission differences for each
sector.  Starting from the emission comparisons for all of China in
Sect. 3.1.1, we further compared emissions by province in Sect. 3.1.2
and gridded emissions in Sect. 3.1.3.</p>
      <p id="d1e1577">As shown in Table 1, the activity rates were assigned independently by
two inventories. As a global emission inventory, ECLIPSE mainly relies
on international statistics of IEA. Differently, MIX obtains the
official statistics of energy consumption and industrial output from
NBS (National Bureau of Statistics) or MEP (Ministry of Environmental
Protection) of China. We can expect high independency for the
determination of emission factors between ECLIPSE (GAINS model) and
MIX (MEIC model). As two independently developed inventory models, the
source classification, technology and removal efficiencies of control
facilities in GAINS and MEIC are expected to be different, although
they both refer to up-to-date measurements and peer-reviewed
data. Different methods were developed in two inventory models for
specific sectors, including power plants, transportation, and
agriculture. For power plants, the spatial proxies were essentially
consistent between ECLIPSE and MIX. For other sectors, emissions were
gridded independently by two emission inventories (see Table S1).</p>
<sec id="Ch1.S3.SS1.SSS1">
  <title>China's emissions by sectors</title>
      <p id="d1e1585">Although a comprehensive dataset on fuel consumption and product yield,
surveys on technique penetration and measurements of emission
factors are incorporated in the inventories, there are several
additional assumptions made to characterize some sources for which
information is either incomplete or missing. For ECLIPSE and MIX,
assumptions are made independently and data sources are often
different. Particularly, MEIC developed high-resolution emissions
based on unit-based information for the power sector and county-level
emissions for transportation.</p>
      <p id="d1e1588">Figure 1 shows the comparisons of China's emission estimates in 2005 and 2010
between two inventories for four key sectors: power, industry, residential
and transportation. For 2010, ECLIPSE estimates about 28 <inline-formula><mml:math id="M85" display="inline"><mml:mi mathvariant="normal">Tg</mml:mi></mml:math></inline-formula> of
<inline-formula><mml:math id="M86" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> and 22 <inline-formula><mml:math id="M87" display="inline"><mml:mi mathvariant="normal">Tg</mml:mi></mml:math></inline-formula> of <inline-formula><mml:math id="M88" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> (expressed in
Tg <inline-formula><mml:math id="M89" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">NO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> hereafter);
1 and 16 % less than MIX, respectively. On a sector level, a 40 %
difference is found for power plants (higher in ECLIPSE), 24 % for the
industry sector (lower in ECLIPSE) for <inline-formula><mml:math id="M90" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>, and
<inline-formula><mml:math id="M91" display="inline"><mml:mrow><mml:mn mathvariant="normal">15</mml:mn><mml:mo>-</mml:mo><mml:mo>-</mml:mo><mml:mn mathvariant="normal">21</mml:mn></mml:mrow></mml:math></inline-formula> % in
power and transportation for <inline-formula><mml:math id="M92" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> (lower in ECLIPSE). It should be
noted that heating plants are distributed in the power and industry sectors
in ECLIPSE, while they are aggregated into industry and residential based on
the plant type of fuel combusted in MIX. Redistributing the heating emissions
by aggregating the heating emissions from the industry and residential
sectors to the power sector in MIX will reduce the differences to about
11 % (higher in ECLIPSE) in the power sector and 17 % (lower in
ECLIPSE) in industry, while increasing the difference in the residential
sector from about 10 to 32 % for <inline-formula><mml:math id="M93" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> and broadening the
differences in the power sector to around 30 % for <inline-formula><mml:math id="M94" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>
(ECLIPSE lower).</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F1" specific-use="star"><caption><p id="d1e1699">Emissions of <inline-formula><mml:math id="M95" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> and <inline-formula><mml:math id="M96" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> in 2005 and 2010
by sector over China. <inline-formula><mml:math id="M97" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> emissions are shown in Tg <inline-formula><mml:math id="M98" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">NO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>.</p></caption>
            <?xmltex \igopts{width=312.980315pt}?><graphic xlink:href="https://acp.copernicus.org/articles/18/3433/2018/acp-18-3433-2018-f01.png"/>

          </fig>

      <p id="d1e1752">As shown in Fig. 1, emission trends from 2005 to 2010 are similar in
two inventories, indicating analogous assumptions of technology
evolution driven by economic growth and implemented air quality
policies in ECLIPSE and MIX.  In general, MIX estimates larger changes
by sectors in the analyzed period.  Specifically, for power plants,
MIX estimates a decline for <inline-formula><mml:math id="M99" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> by 54 %, comparable to the
45 % reduction in ECLIPSE, while for <inline-formula><mml:math id="M100" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> both models
calculate about a 10 % increase. MIX estimates slightly larger
increasing trends for industrial emissions. For <inline-formula><mml:math id="M101" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>
emissions from transport, ECLIPSE calculates lower overall emissions
but higher growth, 26 %, compared to 15 % in MIX.</p>
      <p id="d1e1789">The fuel consumptions of MIX and ECLIPSE among different sectors in
2010 are presented in Table S2. Owing to different source structure in
each of the models, there are sometimes significant discrepancies for
specific sectors.  For example, for coal, the total consumption is
relatively consistent, within 10 % on a mass basis, while in the road
transport sector MIX has 28 % higher diesel fuel use. More details
along with discussion of emissions and implied emission factors are
provided below.</p>
</sec>
<sec id="Ch1.S3.SS1.SSSx1" specific-use="unnumbered">
  <title>Coal-fired power plants</title>
      <p id="d1e1798">For power plants, coal combustion contributes more than 95 % of
<inline-formula><mml:math id="M102" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> and <inline-formula><mml:math id="M103" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> emissions. Activity rates, assumed
heating values, capital sizes, emissions, and key parameters for
determining emission factors for coal-fired power plants are listed
and compared in Table 2.</p>

<?xmltex \floatpos{t}?><table-wrap id="Ch1.T2" specific-use="star"><caption><p id="d1e1826">Activity rates, emissions and emission factors for
<inline-formula><mml:math id="M104" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> and <inline-formula><mml:math id="M105" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> in power plants of
China for 2005 and 2010<inline-formula><mml:math id="M106" display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">a</mml:mi></mml:msup></mml:math></inline-formula>.</p></caption><oasis:table frame="topbot"><oasis:tgroup cols="6">
     <oasis:colspec colnum="1" colname="col1" align="left"/>
     <oasis:colspec colnum="2" colname="col2" align="justify" colwidth="140pt"/>
     <oasis:colspec colnum="3" colname="col3" align="left"/>
     <oasis:colspec colnum="4" colname="col4" align="left" colsep="1"/>
     <oasis:colspec colnum="5" colname="col5" align="left"/>
     <oasis:colspec colnum="6" colname="col6" align="left"/>
     <oasis:thead>
       <oasis:row>  
         <oasis:entry colname="col1">Category</oasis:entry>  
         <oasis:entry colname="col2">Subcategory</oasis:entry>  
         <oasis:entry rowsep="1" namest="col3" nameend="col4" align="center" colsep="1">ECLIPSE </oasis:entry>  
         <oasis:entry rowsep="1" namest="col5" nameend="col6" align="center">MIX </oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">  
         <oasis:entry colname="col1"/>  
         <oasis:entry colname="col2"/>  
         <oasis:entry colname="col3">2005</oasis:entry>  
         <oasis:entry colname="col4">2010</oasis:entry>  
         <oasis:entry colname="col5">2005</oasis:entry>  
         <oasis:entry colname="col6">2010</oasis:entry>
       </oasis:row>
     </oasis:thead>
     <oasis:tbody>
       <oasis:row>  
         <oasis:entry colname="col1">Activity rates</oasis:entry>  
         <oasis:entry colname="col2">Heating value, <inline-formula><mml:math id="M118" display="inline"><mml:mrow><mml:mi mathvariant="normal">MJ</mml:mi><mml:mspace linebreak="nobreak" width="0.125em"/><mml:msup><mml:mi mathvariant="normal">kg</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula></oasis:entry>  
         <oasis:entry colname="col3">20.7</oasis:entry>  
         <oasis:entry colname="col4">20.7</oasis:entry>  
         <oasis:entry colname="col5">19.0<inline-formula><mml:math id="M119" display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">b</mml:mi></mml:msup></mml:math></inline-formula></oasis:entry>  
         <oasis:entry colname="col6">18.8<inline-formula><mml:math id="M120" display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">b</mml:mi></mml:msup></mml:math></inline-formula></oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">  
         <oasis:entry colname="col1"/>  
         <oasis:entry colname="col2">Energy consumption, Tg (PJ)</oasis:entry>  
         <oasis:entry colname="col3">1202 (24 890)</oasis:entry>  
         <oasis:entry colname="col4">1743 (36 074)</oasis:entry>  
         <oasis:entry colname="col5">1055 (20 084)</oasis:entry>  
         <oasis:entry colname="col6">1577 (29 758)</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1">Capacity size</oasis:entry>  
         <oasis:entry colname="col2"><inline-formula><mml:math id="M121" display="inline"><mml:mrow><mml:mo>&lt;</mml:mo><mml:mn mathvariant="normal">100</mml:mn></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math id="M122" display="inline"><mml:mi mathvariant="normal">MW</mml:mi></mml:math></inline-formula></oasis:entry>  
         <oasis:entry colname="col3">39.9 %<inline-formula><mml:math id="M123" display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">c</mml:mi></mml:msup></mml:math></inline-formula></oasis:entry>  
         <oasis:entry colname="col4">5.1 %<inline-formula><mml:math id="M124" display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">c</mml:mi></mml:msup></mml:math></inline-formula></oasis:entry>  
         <oasis:entry colname="col5">25.0 %</oasis:entry>  
         <oasis:entry colname="col6">11.5 %</oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">  
         <oasis:entry colname="col1"/>  
         <oasis:entry colname="col2"><inline-formula><mml:math id="M125" display="inline"><mml:mrow><mml:mo>≥</mml:mo><mml:mn mathvariant="normal">100</mml:mn></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math id="M126" display="inline"><mml:mi mathvariant="normal">MW</mml:mi></mml:math></inline-formula></oasis:entry>  
         <oasis:entry colname="col3">60.1 %</oasis:entry>  
         <oasis:entry colname="col4">94.9 %</oasis:entry>  
         <oasis:entry colname="col5">75.0 %</oasis:entry>  
         <oasis:entry colname="col6">88.5 %</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1"><inline-formula><mml:math id="M127" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> emissions and</oasis:entry>  
         <oasis:entry colname="col2"><inline-formula><mml:math id="M128" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> emissions, Gg</oasis:entry>  
         <oasis:entry colname="col3">19 528</oasis:entry>  
         <oasis:entry colname="col4">10 645</oasis:entry>  
         <oasis:entry colname="col5">16 516</oasis:entry>  
         <oasis:entry colname="col6">7754</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1">emission factors</oasis:entry>  
         <oasis:entry colname="col2">Average <inline-formula><mml:math id="M129" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> emission factor,  <inline-formula><mml:math id="M130" display="inline"><mml:mrow><mml:mi mathvariant="normal">g</mml:mi><mml:mspace width="0.125em" linebreak="nobreak"/><mml:msup><mml:mi mathvariant="normal">kg</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula> (<inline-formula><mml:math id="M131" display="inline"><mml:mrow><mml:mi mathvariant="normal">g</mml:mi><mml:mspace width="0.125em" linebreak="nobreak"/><mml:msup><mml:mi mathvariant="normal">MJ</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>)</oasis:entry>  
         <oasis:entry colname="col3">16.2 (0.79)</oasis:entry>  
         <oasis:entry colname="col4">6.11 (0.29)</oasis:entry>  
         <oasis:entry colname="col5">15.6 (0.82)</oasis:entry>  
         <oasis:entry colname="col6">4.92 (0.26)</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1"/>  
         <oasis:entry colname="col2">Sulfur content, %</oasis:entry>  
         <oasis:entry colname="col3">1.13</oasis:entry>  
         <oasis:entry colname="col4">1.13</oasis:entry>  
         <oasis:entry colname="col5">1.04</oasis:entry>  
         <oasis:entry colname="col6">0.95</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1"/>  
         <oasis:entry colname="col2">Sulfur retention in ashes, %</oasis:entry>  
         <oasis:entry colname="col3">0.092</oasis:entry>  
         <oasis:entry colname="col4">0.092</oasis:entry>  
         <oasis:entry colname="col5">0.15</oasis:entry>  
         <oasis:entry colname="col6">0.15</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1"/>  
         <oasis:entry colname="col2">Raw <inline-formula><mml:math id="M132" display="inline"><mml:mrow><mml:msub><mml:mtext>EF</mml:mtext><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:msub></mml:mrow></mml:math></inline-formula><inline-formula><mml:math id="M133" display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">d</mml:mi></mml:msup></mml:math></inline-formula>, <inline-formula><mml:math id="M134" display="inline"><mml:mrow><mml:mi mathvariant="normal">g</mml:mi><mml:mspace width="0.125em" linebreak="nobreak"/><mml:msup><mml:mi mathvariant="normal">kg</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula></oasis:entry>  
         <oasis:entry colname="col3">22.5</oasis:entry>  
         <oasis:entry colname="col4">22.5</oasis:entry>  
         <oasis:entry colname="col5">20.8</oasis:entry>  
         <oasis:entry colname="col6">19.0</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1"/>  
         <oasis:entry colname="col2">Removal efficiency of FGD, %</oasis:entry>  
         <oasis:entry colname="col3">95</oasis:entry>  
         <oasis:entry colname="col4">95</oasis:entry>  
         <oasis:entry colname="col5">80</oasis:entry>  
         <oasis:entry colname="col6">80</oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">  
         <oasis:entry colname="col1"/>  
         <oasis:entry colname="col2">Application rate of FGD, %</oasis:entry>  
         <oasis:entry colname="col3">17.6</oasis:entry>  
         <oasis:entry colname="col4">65.4</oasis:entry>  
         <oasis:entry colname="col5">12.6</oasis:entry>  
         <oasis:entry colname="col6">87.0</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1"><inline-formula><mml:math id="M135" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> emissions and</oasis:entry>  
         <oasis:entry colname="col2"><inline-formula><mml:math id="M136" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> emissions, Gg</oasis:entry>  
         <oasis:entry colname="col3">6131</oasis:entry>  
         <oasis:entry colname="col4">7090</oasis:entry>  
         <oasis:entry colname="col5">6561</oasis:entry>  
         <oasis:entry colname="col6">8302</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1">emission factors</oasis:entry>  
         <oasis:entry colname="col2">Average <inline-formula><mml:math id="M137" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> emission factor,  <inline-formula><mml:math id="M138" display="inline"><mml:mrow><mml:mi mathvariant="normal">g</mml:mi><mml:mspace width="0.125em" linebreak="nobreak"/><mml:msup><mml:mi mathvariant="normal">kg</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula> (<inline-formula><mml:math id="M139" display="inline"><mml:mrow><mml:mi mathvariant="normal">g</mml:mi><mml:mspace linebreak="nobreak" width="0.125em"/><mml:msup><mml:mi mathvariant="normal">MJ</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>)</oasis:entry>  
         <oasis:entry colname="col3">5.10 (0.25)</oasis:entry>  
         <oasis:entry colname="col4">4.07 (0.20)</oasis:entry>  
         <oasis:entry colname="col5">6.22 (0.33)</oasis:entry>  
         <oasis:entry colname="col6">5.27 (0.28)</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1"/>  
         <oasis:entry colname="col2">LNB penetration, %</oasis:entry>  
         <oasis:entry colname="col3">29.4</oasis:entry>  
         <oasis:entry colname="col4">30.1</oasis:entry>  
         <oasis:entry colname="col5">53.7</oasis:entry>  
         <oasis:entry colname="col6">81.4</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1"/>  
         <oasis:entry colname="col2">Unabated <inline-formula><mml:math id="M140" display="inline"><mml:mrow><mml:msub><mml:mtext>EF</mml:mtext><mml:mtext>nox</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>, existing large PP, <inline-formula><mml:math id="M141" display="inline"><mml:mrow><mml:mi mathvariant="normal">g</mml:mi><mml:mspace width="0.125em" linebreak="nobreak"/><mml:msup><mml:mi mathvariant="normal">kg</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula></oasis:entry>  
         <oasis:entry colname="col3">7.55</oasis:entry>  
         <oasis:entry colname="col4">7.55</oasis:entry>  
         <oasis:entry colname="col5">7.21</oasis:entry>  
         <oasis:entry colname="col6">7.21</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1"/>  
         <oasis:entry colname="col2">Unabated <inline-formula><mml:math id="M142" display="inline"><mml:mrow><mml:msub><mml:mtext>EF</mml:mtext><mml:mtext>nox</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>, existing small PP, <inline-formula><mml:math id="M143" display="inline"><mml:mrow><mml:mi mathvariant="normal">g</mml:mi><mml:mspace width="0.125em" linebreak="nobreak"/><mml:msup><mml:mi mathvariant="normal">kg</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula></oasis:entry>  
         <oasis:entry colname="col3">7.04</oasis:entry>  
         <oasis:entry colname="col4">7.04</oasis:entry>  
         <oasis:entry colname="col5">8.96</oasis:entry>  
         <oasis:entry colname="col6">8.96</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1"/>  
         <oasis:entry colname="col2">LNB <inline-formula><mml:math id="M144" display="inline"><mml:mrow><mml:msub><mml:mtext>EF</mml:mtext><mml:mtext>nox</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>, existing large PP, <inline-formula><mml:math id="M145" display="inline"><mml:mrow><mml:mi mathvariant="normal">g</mml:mi><mml:mspace width="0.125em" linebreak="nobreak"/><mml:msup><mml:mi mathvariant="normal">kg</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula></oasis:entry>  
         <oasis:entry colname="col3">3.78</oasis:entry>  
         <oasis:entry colname="col4">3.78</oasis:entry>  
         <oasis:entry colname="col5">5.63</oasis:entry>  
         <oasis:entry colname="col6">5.63</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1"/>  
         <oasis:entry colname="col2">LNB <inline-formula><mml:math id="M146" display="inline"><mml:mrow><mml:msub><mml:mtext>EF</mml:mtext><mml:mtext>nox</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>, existing small PP, <inline-formula><mml:math id="M147" display="inline"><mml:mrow><mml:mi mathvariant="normal">g</mml:mi><mml:mspace linebreak="nobreak" width="0.125em"/><mml:msup><mml:mi mathvariant="normal">kg</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula></oasis:entry>  
         <oasis:entry colname="col3">3.52</oasis:entry>  
         <oasis:entry colname="col4">3.52</oasis:entry>  
         <oasis:entry colname="col5">7.00</oasis:entry>  
         <oasis:entry colname="col6">7.00</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1"/>  
         <oasis:entry colname="col2">LNB <inline-formula><mml:math id="M148" display="inline"><mml:mrow><mml:msub><mml:mtext>EF</mml:mtext><mml:mtext>nox</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>, newly built PP, <inline-formula><mml:math id="M149" display="inline"><mml:mrow><mml:mi mathvariant="normal">g</mml:mi><mml:mspace width="0.125em" linebreak="nobreak"/><mml:msup><mml:mi mathvariant="normal">kg</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula></oasis:entry>  
         <oasis:entry colname="col3">3.11</oasis:entry>  
         <oasis:entry colname="col4">3.11</oasis:entry>  
         <oasis:entry colname="col5">4.21</oasis:entry>  
         <oasis:entry colname="col6">4.21</oasis:entry>
       </oasis:row>
     </oasis:tbody>
   </oasis:tgroup></oasis:table><table-wrap-foot><p id="d1e1860"><inline-formula><mml:math id="M107" display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">a</mml:mi></mml:msup></mml:math></inline-formula> Including both raw coal and derived coal.<?xmltex \hack{\\}?><inline-formula><mml:math id="M108" display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">b</mml:mi></mml:msup></mml:math></inline-formula> National average.<?xmltex \hack{\\}?><inline-formula><mml:math id="M109" display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">c</mml:mi></mml:msup></mml:math></inline-formula> We interpret the defined small units (<inline-formula><mml:math id="M110" display="inline"><mml:mrow><mml:mo>&lt;</mml:mo><mml:mn mathvariant="normal">50</mml:mn></mml:mrow></mml:math></inline-formula> MW) in ECLIPSE to <inline-formula><mml:math id="M111" display="inline"><mml:mrow><mml:mo>&lt;</mml:mo><mml:mn mathvariant="normal">100</mml:mn></mml:mrow></mml:math></inline-formula> MW
here by assuming that <inline-formula><mml:math id="M112" display="inline"><mml:mrow><mml:mn mathvariant="normal">1</mml:mn><mml:mo>/</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:math></inline-formula> of the units in the range of <inline-formula><mml:math id="M113" display="inline"><mml:mrow><mml:mo>&lt;</mml:mo><mml:mn mathvariant="normal">100</mml:mn></mml:mrow></mml:math></inline-formula> MW fall into <inline-formula><mml:math id="M114" display="inline"><mml:mrow><mml:mo>&lt;</mml:mo><mml:mn mathvariant="normal">50</mml:mn></mml:mrow></mml:math></inline-formula> MW according to Liu et al. (2015).<?xmltex \hack{\\}?><inline-formula><mml:math id="M115" display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">d</mml:mi></mml:msup></mml:math></inline-formula> The raw <inline-formula><mml:math id="M116" display="inline"><mml:mrow><mml:msub><mml:mtext>EF</mml:mtext><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:msub></mml:mrow></mml:math></inline-formula> is calculated following
<inline-formula><mml:math id="M117" display="inline"><mml:mrow><mml:mtext>EF</mml:mtext><mml:mo>=</mml:mo><mml:mn mathvariant="normal">2</mml:mn><mml:mo>×</mml:mo><mml:mtext>sulfur content</mml:mtext><mml:mo>×</mml:mo><mml:mo>(</mml:mo><mml:mn mathvariant="normal">1</mml:mn><mml:mo>-</mml:mo><mml:mtext>sulfur
retention in ashes</mml:mtext><mml:mo>)</mml:mo></mml:mrow></mml:math></inline-formula>.</p></table-wrap-foot></table-wrap>

      <p id="d1e2847">The coal consumption of ECLIPSE is <inline-formula><mml:math id="M150" display="inline"><mml:mrow><mml:mn mathvariant="normal">11</mml:mn><mml:mo>-</mml:mo><mml:mo>-</mml:mo><mml:mn mathvariant="normal">14</mml:mn></mml:mrow></mml:math></inline-formula> % higher than MIX in 2005 and 2010
(mass based) due to the differences in energy statistics and included
sources. As a global emission inventory model, ECLIPSE (GAINS model) relies
on the energy statistics from IEA (<uri>http://www.iea.org/</uri>), consistent
with the national Energy Balance Sheets provided by the NBS of China (Hong
et al., 2017), and also includes district heating plants. In MIX (MEIC
model), coal consumption in power plants is derived from CPED, which contains
the detailed fuel consumption rates, fuel quality, combustion and control
technology of over 7600 power-generating units in China (Liu et al., 2015).
It should be noted that the heating values of coal in China declined between
2005 and 2010, based on the CPED database (Liu et al., 2015).</p>
      <p id="d1e2867">ECLIPSE's <inline-formula><mml:math id="M151" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> emissions are 37 and 18 % higher than MIX in
2010 and 2005, respectively. In 2010, the implied <inline-formula><mml:math id="M152" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> emission
factor is determined as 6.1 <inline-formula><mml:math id="M153" display="inline"><mml:mrow><mml:mi mathvariant="normal">g</mml:mi><mml:mspace linebreak="nobreak" width="0.125em"/><mml:msup><mml:mi mathvariant="normal">kg</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>, 24 % higher than
4.9 <inline-formula><mml:math id="M154" display="inline"><mml:mrow><mml:mi mathvariant="normal">g</mml:mi><mml:mspace linebreak="nobreak" width="0.125em"/><mml:msup><mml:mi mathvariant="normal">kg</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula> estimated by MIX. As shown in Table 2, raw
emission factor, FGD application rate and removal efficiency all
contribute to this discrepancy. <inline-formula><mml:math id="M155" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> raw emission factor of
ECLIPSE is 19 % higher than MIX due to different coal quality
assumed in two inventory models. MIX assumes higher FGD penetration (87.0 % vs. 65.4 %) but lower removal
efficiency (80 % vs. 95 %)
than ECLIPSE. From 2005 to 2010, the emission
discrepancy grew larger because of the decrease in sulfur content and
sharply increasing application rates of FGD.</p>
      <p id="d1e2938">For <inline-formula><mml:math id="M156" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>, the emission estimates of power plants are
similar between ECLIPSE and MIX: 7 % difference in 2005 and
15 % in 2010. Compared to MIX, the lower emission estimates of
ECLIPSE are primarily due to emission factors, which are about
20 % lower and can be explained by three factors:
<list list-type="custom"><list-item><label>(a)</label><p id="d1e2953"><italic>Fuel distributions between large and small units</italic>.
In MIX, about 89 % of coal was consumed by large or medium
units (<inline-formula><mml:math id="M157" display="inline"><mml:mrow><mml:mo>&gt;</mml:mo><mml:mn mathvariant="normal">100</mml:mn></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math id="M158" display="inline"><mml:mi mathvariant="normal">MW</mml:mi></mml:math></inline-formula>) in 2010, compared to 95 % in ECLIPSE,
reflecting different interpretations of mitigation strategies during the
11th Five-Year Plan of China.</p></list-item><list-item><label>(b)</label><p id="d1e2975"><italic>Raw emission factors by technologies</italic>. The unabated
emission factor of <inline-formula><mml:math id="M159" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> for existing large power plants
differs within 5 %, while for plants with LNBs
(low-<inline-formula><mml:math id="M160" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> burners), emission factors are 33 % lower
in ECLIPSE. Furthermore, compared to MIX, ECLIPSE used 21 %
lower emission factors for small plants and 26 % lower emission factors for
newly built plants.</p></list-item><list-item><label>(c)</label><p id="d1e3002"><italic>Application rates of technologies</italic>. MIX assumes
that in 2010 81 % of power plants are equipped with the LNB
techniques while only a 30 % application rate is considered in
ECLIPSE. The impact of this difference is partly offset by higher
efficiencies of LNB assumed in the latter. Neither model assumed the
implementation of selective catalytic reduction installations in this period.</p></list-item></list></p>
</sec>
<sec id="Ch1.S3.SS1.SSSx2" specific-use="unnumbered">
  <title>Industry</title>
      <p id="d1e3014">Comparison of industrial emissions is most challenging since this
sector includes a multitude of sources with greatly varying emission
characteristics and different representation in the investigated
inventories. Overall, ECLIPSE calculates lower emissions, i.e., 24 and
13 % for <inline-formula><mml:math id="M161" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> and <inline-formula><mml:math id="M162" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> in 2010 and 22 and
0.1 % in 2005, respectively<inline-formula><mml:math id="M163" display="inline"><mml:msub><mml:mi/><mml:mrow><mml:mo>.</mml:mo><mml:mspace linebreak="nobreak" width="0.125em"/></mml:mrow></mml:msub></mml:math></inline-formula>We compare the parameters of
the main contributing industrial sources below keeping the source
classification differences in mind.</p>
      <p id="d1e3050"><italic>Coal-fired industrial boilers</italic>. MIX estimates about
10.4 <inline-formula><mml:math id="M164" display="inline"><mml:mi mathvariant="normal">Tg</mml:mi></mml:math></inline-formula> of <inline-formula><mml:math id="M165" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> and 4.3 <inline-formula><mml:math id="M166" display="inline"><mml:mi mathvariant="normal">Tg</mml:mi></mml:math></inline-formula> of <inline-formula><mml:math id="M167" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> emitted from
combustion in industrial boilers, nearly 123 and 71 % more than
ECLIPSE. Including fuel use in fuel conversion and the transformation
sector in ECLIPSE slightly reduces the discrepancy to 101 % for
<inline-formula><mml:math id="M168" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> and 70 % for <inline-formula><mml:math id="M169" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>. While coal consumption
of MIX is 29 % larger than ECLIPSE, the key factor contributing to the
difference is varying emission factors.</p>
      <p id="d1e3114"><italic>Production of cement and brick</italic>. Cement production is among
the major industrial sources, contributing more than 26 % of industrial
emissions. Both inventories use the same cement production rates,
while ECLIPSE applies higher emission factors leading to 13 and
29 % higher <inline-formula><mml:math id="M170" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> and <inline-formula><mml:math id="M171" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> emissions than MIX for
2010. For brick production, the ECLIPSE emission estimates of
<inline-formula><mml:math id="M172" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> and <inline-formula><mml:math id="M173" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> are more than 3 times higher with a
difference in production rate of only 25 %.  This sector,
however, is very uncertain, as information about fuel use is poorly
known and actual emission factors are missing.</p>
      <p id="d1e3163"><italic>Other sources</italic>. One of major reasons for discrepancy is due to
oil combustion in the industrial sector where ECLIPSE assumptions indicate
about 36 % lower use than MIX, resulting in the 30 %
differences for <inline-formula><mml:math id="M174" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> and <inline-formula><mml:math id="M175" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> emissions.  Another
systematic issue is allocation of emissions between furnaces and the
production process, where for sectors like pulp and paper, nonferrous
metal production, sinter and lime production, etc., different
approaches are used in the GAINS (ECLIPSE) and MEIC (MIX) models.</p>
</sec>
<sec id="Ch1.S3.SS1.SSSx3" specific-use="unnumbered">
  <title>Residential</title>
      <p id="d1e3196">Residential combustion contributes around <inline-formula><mml:math id="M176" display="inline"><mml:mrow><mml:mn mathvariant="normal">10</mml:mn><mml:mo>-</mml:mo><mml:mn mathvariant="normal">15</mml:mn></mml:mrow></mml:math></inline-formula> % of
<inline-formula><mml:math id="M177" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> and 6 % of <inline-formula><mml:math id="M178" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> emissions in the considered
period. The emission estimates are comparable between two inventories,
for example for 2010, 4.15 <inline-formula><mml:math id="M179" display="inline"><mml:mi mathvariant="normal">Tg</mml:mi></mml:math></inline-formula> of <inline-formula><mml:math id="M180" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> and 1.73 <inline-formula><mml:math id="M181" display="inline"><mml:mi mathvariant="normal">Tg</mml:mi></mml:math></inline-formula>
of <inline-formula><mml:math id="M182" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> in ECLIPSE and 4.58 <inline-formula><mml:math id="M183" display="inline"><mml:mi mathvariant="normal">Tg</mml:mi></mml:math></inline-formula> of <inline-formula><mml:math id="M184" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>, 1.38 <inline-formula><mml:math id="M185" display="inline"><mml:mi mathvariant="normal">Tg</mml:mi></mml:math></inline-formula> of
<inline-formula><mml:math id="M186" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> in MIX. Both models use nearly identical coal
consumptions: about 302 <inline-formula><mml:math id="M187" display="inline"><mml:mi mathvariant="normal">Tg</mml:mi></mml:math></inline-formula> (ECLIPSE) and 306 <inline-formula><mml:math id="M188" display="inline"><mml:mi mathvariant="normal">Tg</mml:mi></mml:math></inline-formula> (MIX),
indicating the consistent statistics from the provincial energy balance
table and the national ones for fuel consumed in residential
boilers and/or stoves.</p>
</sec>
<sec id="Ch1.S3.SS1.SSSx4" specific-use="unnumbered">
  <title>Transportation</title>
      <p id="d1e3327">Transportation sector contributes more than 25 % to the total
<inline-formula><mml:math id="M189" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> emissions, but is negligible for <inline-formula><mml:math id="M190" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> emissions. In
ECLIPSE, high emitters representing an old and poorly maintained vehicle
fleet share 12 % of the total transport emissions. ECLIPSE
estimates 5.50 <inline-formula><mml:math id="M191" display="inline"><mml:mi mathvariant="normal">Tg</mml:mi></mml:math></inline-formula> of <inline-formula><mml:math id="M192" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> emissions in 2010
(4.86 <inline-formula><mml:math id="M193" display="inline"><mml:mi mathvariant="normal">Tg</mml:mi></mml:math></inline-formula> as shown in Table 3 and 0.64 <inline-formula><mml:math id="M194" display="inline"><mml:mi mathvariant="normal">Tg</mml:mi></mml:math></inline-formula> from
high emitters), 21 % less than MIX. While the ECLIPSE inventory
includes province-specific fleet characteristics (Klimont et al.,
2017), MIX emissions were developed at a county level by modeling the
vehicle stock following the Gompertz function, technology
distributions in accordance with emission standards and emission
factors using an international vehicle emission model, as
documented by Zheng et al. (2014).</p>

<?xmltex \floatpos{t}?><table-wrap id="Ch1.T3" specific-use="star"><caption><p id="d1e3388">Comparisons of activity, emissions and emission factors
for the transport sector emission estimates of
<inline-formula><mml:math id="M195" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula><inline-formula><mml:math id="M196" display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">a</mml:mi></mml:msup></mml:math></inline-formula>.</p></caption><oasis:table frame="topbot"><?xmltex \begin{scaleboxenv}{.85}[.85]?><oasis:tgroup cols="10">
     <oasis:colspec colnum="1" colname="col1" align="left"/>
     <oasis:colspec colnum="2" colname="col2" align="left"/>
     <oasis:colspec colnum="3" colname="col3" align="right"/>
     <oasis:colspec colnum="4" colname="col4" align="right"/>
     <oasis:colspec colnum="5" colname="col5" align="right"/>
     <oasis:colspec colnum="6" colname="col6" align="right"/>
     <oasis:colspec colnum="7" colname="col7" align="right"/>
     <oasis:colspec colnum="8" colname="col8" align="right"/>
     <oasis:colspec colnum="9" colname="col9" align="right"/>
     <oasis:colspec colnum="10" colname="col10" align="right"/>
     <oasis:thead>
       <oasis:row>  
         <oasis:entry colname="col1">Items</oasis:entry>  
         <oasis:entry colname="col2">Inventory-year</oasis:entry>  
         <oasis:entry colname="col3">HDV-G</oasis:entry>  
         <oasis:entry colname="col4">LDV-G</oasis:entry>  
         <oasis:entry colname="col5">MC</oasis:entry>  
         <oasis:entry colname="col6">All gasoline</oasis:entry>  
         <oasis:entry colname="col7">HDV-D</oasis:entry>  
         <oasis:entry colname="col8">LDV-D</oasis:entry>  
         <oasis:entry colname="col9">All diesel</oasis:entry>  
         <oasis:entry colname="col10">Diesel</oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">  
         <oasis:entry colname="col1"/>  
         <oasis:entry colname="col2"/>  
         <oasis:entry colname="col3"/>  
         <oasis:entry colname="col4"/>  
         <oasis:entry colname="col5"/>  
         <oasis:entry colname="col6">on-road</oasis:entry>  
         <oasis:entry colname="col7"/>  
         <oasis:entry colname="col8"/>  
         <oasis:entry colname="col9">on-road</oasis:entry>  
         <oasis:entry colname="col10">off-road</oasis:entry>
       </oasis:row>
     </oasis:thead>
     <oasis:tbody>
       <oasis:row>  
         <oasis:entry colname="col1">Fuel consumptions,</oasis:entry>  
         <oasis:entry colname="col2">ECL-2005</oasis:entry>  
         <oasis:entry colname="col3">3.63</oasis:entry>  
         <oasis:entry colname="col4">35.0</oasis:entry>  
         <oasis:entry colname="col5">8.57</oasis:entry>  
         <oasis:entry colname="col6">47.2</oasis:entry>  
         <oasis:entry colname="col7">29.7</oasis:entry>  
         <oasis:entry colname="col8">12.8</oasis:entry>  
         <oasis:entry colname="col9">42.5</oasis:entry>  
         <oasis:entry colname="col10">23.1</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1">Tg</oasis:entry>  
         <oasis:entry colname="col2">ECL-2010</oasis:entry>  
         <oasis:entry colname="col3">1.50</oasis:entry>  
         <oasis:entry colname="col4">62.4</oasis:entry>  
         <oasis:entry colname="col5">7.03</oasis:entry>  
         <oasis:entry colname="col6">71.0</oasis:entry>  
         <oasis:entry colname="col7">51.0</oasis:entry>  
         <oasis:entry colname="col8">20.9</oasis:entry>  
         <oasis:entry colname="col9">72.0</oasis:entry>  
         <oasis:entry colname="col10">25.8</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1"/>  
         <oasis:entry colname="col2">MIX-2005</oasis:entry>  
         <oasis:entry colname="col3">13.3</oasis:entry>  
         <oasis:entry colname="col4">25.1</oasis:entry>  
         <oasis:entry colname="col5">8.30</oasis:entry>  
         <oasis:entry colname="col6">46.7</oasis:entry>  
         <oasis:entry colname="col7">59.7</oasis:entry>  
         <oasis:entry colname="col8">6.11</oasis:entry>  
         <oasis:entry colname="col9">65.8</oasis:entry>  
         <oasis:entry colname="col10">35.2</oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">  
         <oasis:entry colname="col1"/>  
         <oasis:entry colname="col2">MIX-2010</oasis:entry>  
         <oasis:entry colname="col3">5.76</oasis:entry>  
         <oasis:entry colname="col4">52.8</oasis:entry>  
         <oasis:entry colname="col5">10.3</oasis:entry>  
         <oasis:entry colname="col6">68.9</oasis:entry>  
         <oasis:entry colname="col7">81.2</oasis:entry>  
         <oasis:entry colname="col8">11.0</oasis:entry>  
         <oasis:entry colname="col9">92.2</oasis:entry>  
         <oasis:entry colname="col10">42.1</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1"><inline-formula><mml:math id="M201" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> emissions,</oasis:entry>  
         <oasis:entry colname="col2">ECL-2005<inline-formula><mml:math id="M202" display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">b</mml:mi></mml:msup></mml:math></inline-formula></oasis:entry>  
         <oasis:entry colname="col3">109</oasis:entry>  
         <oasis:entry colname="col4">722</oasis:entry>  
         <oasis:entry colname="col5">46</oasis:entry>  
         <oasis:entry colname="col6">878</oasis:entry>  
         <oasis:entry colname="col7">1570</oasis:entry>  
         <oasis:entry colname="col8">193</oasis:entry>  
         <oasis:entry colname="col9">1762</oasis:entry>  
         <oasis:entry colname="col10">1166</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1">Gg</oasis:entry>  
         <oasis:entry colname="col2">ECL-2010<inline-formula><mml:math id="M203" display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">b</mml:mi></mml:msup></mml:math></inline-formula></oasis:entry>  
         <oasis:entry colname="col3">27</oasis:entry>  
         <oasis:entry colname="col4">582</oasis:entry>  
         <oasis:entry colname="col5">34</oasis:entry>  
         <oasis:entry colname="col6">643</oasis:entry>  
         <oasis:entry colname="col7">2667</oasis:entry>  
         <oasis:entry colname="col8">335</oasis:entry>  
         <oasis:entry colname="col9">3002</oasis:entry>  
         <oasis:entry colname="col10">1215</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1"/>  
         <oasis:entry colname="col2">MIX-2005</oasis:entry>  
         <oasis:entry colname="col3">208</oasis:entry>  
         <oasis:entry colname="col4">314</oasis:entry>  
         <oasis:entry colname="col5">129</oasis:entry>  
         <oasis:entry colname="col6">652</oasis:entry>  
         <oasis:entry colname="col7">3170</oasis:entry>  
         <oasis:entry colname="col8">398</oasis:entry>  
         <oasis:entry colname="col9">3568</oasis:entry>  
         <oasis:entry colname="col10">1854</oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">  
         <oasis:entry colname="col1"/>  
         <oasis:entry colname="col2">MIX-2010</oasis:entry>  
         <oasis:entry colname="col3">79</oasis:entry>  
         <oasis:entry colname="col4">292</oasis:entry>  
         <oasis:entry colname="col5">92</oasis:entry>  
         <oasis:entry colname="col6">463</oasis:entry>  
         <oasis:entry colname="col7">3614</oasis:entry>  
         <oasis:entry colname="col8">705</oasis:entry>  
         <oasis:entry colname="col9">4319</oasis:entry>  
         <oasis:entry colname="col10">2201</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1">Average <inline-formula><mml:math id="M204" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula></oasis:entry>  
         <oasis:entry colname="col2">ECL-2005<inline-formula><mml:math id="M205" display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">c</mml:mi></mml:msup></mml:math></inline-formula></oasis:entry>  
         <oasis:entry colname="col3">30.1 (0.70)</oasis:entry>  
         <oasis:entry colname="col4">20.6 (0.48)</oasis:entry>  
         <oasis:entry colname="col5">5.4 (0.13)</oasis:entry>  
         <oasis:entry colname="col6">18.6 (0.43)</oasis:entry>  
         <oasis:entry colname="col7">52.8 (1.22)</oasis:entry>  
         <oasis:entry colname="col8">15.1 (0.35)</oasis:entry>  
         <oasis:entry colname="col9">41.4 (0.96)</oasis:entry>  
         <oasis:entry colname="col10">50.4 (1.17)</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1">emission factors,</oasis:entry>  
         <oasis:entry colname="col2">ECL-2010<inline-formula><mml:math id="M206" display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">c</mml:mi></mml:msup></mml:math></inline-formula></oasis:entry>  
         <oasis:entry colname="col3">18.0 (0.42)</oasis:entry>  
         <oasis:entry colname="col4">9.3 (0.22)</oasis:entry>  
         <oasis:entry colname="col5">4.8 (0.11)</oasis:entry>  
         <oasis:entry colname="col6">9.1 (0.21)</oasis:entry>  
         <oasis:entry colname="col7">52.2 (1.21)</oasis:entry>  
         <oasis:entry colname="col8">16.0 (0.37)</oasis:entry>  
         <oasis:entry colname="col9">41.7 (0.97)</oasis:entry>  
         <oasis:entry colname="col10">47.1 (1.09)</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1"><inline-formula><mml:math id="M207" display="inline"><mml:mrow><mml:mi mathvariant="normal">g</mml:mi><mml:mspace width="0.125em" linebreak="nobreak"/><mml:msup><mml:mi mathvariant="normal">kg</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula> (<inline-formula><mml:math id="M208" display="inline"><mml:mrow><mml:mi mathvariant="normal">g</mml:mi><mml:mspace linebreak="nobreak" width="0.125em"/><mml:msup><mml:mi mathvariant="normal">MJ</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>)<inline-formula><mml:math id="M209" display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">b</mml:mi></mml:msup></mml:math></inline-formula></oasis:entry>  
         <oasis:entry colname="col2">MIX-2005</oasis:entry>  
         <oasis:entry colname="col3">15.6 (0.36)</oasis:entry>  
         <oasis:entry colname="col4">12.5 (0.29)</oasis:entry>  
         <oasis:entry colname="col5">15.6 (0.36)</oasis:entry>  
         <oasis:entry colname="col6">14.0 (0.32)</oasis:entry>  
         <oasis:entry colname="col7">53.1 (1.23)</oasis:entry>  
         <oasis:entry colname="col8">65.1 (1.51)</oasis:entry>  
         <oasis:entry colname="col9">54.2 (1.26)</oasis:entry>  
         <oasis:entry colname="col10">52.7 (1.22)</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1"/>  
         <oasis:entry colname="col2">MIX-2010</oasis:entry>  
         <oasis:entry colname="col3">13.7 (0.32)</oasis:entry>  
         <oasis:entry colname="col4">5.5 (0.13)</oasis:entry>  
         <oasis:entry colname="col5">9.0 (0.21)</oasis:entry>  
         <oasis:entry colname="col6">6.7 (0.16)</oasis:entry>  
         <oasis:entry colname="col7">44.5 (1.03)</oasis:entry>  
         <oasis:entry colname="col8">64.1 (1.49)</oasis:entry>  
         <oasis:entry colname="col9">46.8 (1.09)</oasis:entry>  
         <oasis:entry colname="col10">52.3 (1.21)</oasis:entry>
       </oasis:row>
     </oasis:tbody>
   </oasis:tgroup><?xmltex \end{scaleboxenv}?></oasis:table><?xmltex \begin{scaleboxenv}{.85}[.85]?><table-wrap-foot><p id="d1e3410"><?xmltex \hack{\vspace{2mm}}?>
<inline-formula><mml:math id="M197" display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">a</mml:mi></mml:msup></mml:math></inline-formula> HDV-G: heavy-/medium-duty buses and trucks – gasoline
fueled; LDV-G: light-duty buses, trucks and passenger cars –
gasoline fueled; MC: motorcycle; HDV-D: heavy-/medium-duty buses and
trucks – diesel fueled;
LDV-D: light-duty buses and trucks – diesel fueled.<?xmltex \hack{\\}?><inline-formula><mml:math id="M198" display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">b</mml:mi></mml:msup></mml:math></inline-formula> High emitters are not included.<?xmltex \hack{\\}?><inline-formula><mml:math id="M199" display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">c</mml:mi></mml:msup></mml:math></inline-formula> Emission factors on a mass basis are converted to an energy basis with
a heating value of 43.1 <inline-formula><mml:math id="M200" display="inline"><mml:mrow><mml:mi mathvariant="normal">MJ</mml:mi><mml:mspace linebreak="nobreak" width="0.125em"/><mml:msup><mml:mi mathvariant="normal">kg</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula> for gasoline and diesel.</p></table-wrap-foot><?xmltex \end{scaleboxenv}?></table-wrap>

      <p id="d1e4052">Table 3 compares the fuel consumption, emission estimates and net
emission factors among various vehicle types in two inventories for
2005 and 2010.  Parameters for 2005 show a similar difference ratio to
those in 2010.  Assumptions for diesel combustion sources (on-road and
off-road) are the main contributor to emission discrepancies. In 2010,
diesel emissions of ECLIPSE are over 50 % lower than MIX
estimates.</p>
      <p id="d1e4055"><italic>Gasoline</italic>. There is only a 3 % difference in total gasoline
use in the transport sector between ECLIPSE and MIX. However, emission
estimates are significantly different, especially for light-duty
vehicles, which dominate the total. The consistency in the total
gasoline consumption between ECLIPSE and MIX is attributed to the
consistency in statistics. As shown in Table 3, the gasoline
consumptions by vehicle types show large differences between ECLIPSE
and MIX, indicating the different vehicle fleet assumptions in two
inventory models. Detailed data are not known and each of the
inventories (or research groups developing them) relied on their own
assumptions about fuel consumption per vehicle and mileage traveled and
combined those with the available data on the number of vehicles,
their sales and retirement rate.  Owing to the reasons above, the
results can differ significantly. Light-duty vehicles are the largest
gasoline consumer (<inline-formula><mml:math id="M210" display="inline"><mml:mrow><mml:mo>&gt;</mml:mo><mml:mn mathvariant="normal">77</mml:mn></mml:mrow></mml:math></inline-formula> %) in both inventories, with 18 %
higher gasoline consumption estimated in ECLIPSE than those of MIX in
2010. Accordingly, ECLIPSE estimates less gasoline consumed in heavy-duty vehicles (74 %) and motorcycles (32 %) than MIX.  These
differences reduced from 2005 to 2010. Emission estimates of heavy-duty vehicles and motorcycles also show large differences
between two inventories. For heavy-duty vehicles, ECLIPSE estimates lower emissions
than MIX (66 % in 2010), as a result of less fuel consumption,
while higher emission factors are estimated in ECLIPSE. For motorcycles, emissions of ECLIPSE
are 64 % lower than MIX, contributed by both fuel consumption and
emission factors. It appears that the assumptions about penetration
and performance of vehicles with specific emission standards vary
between the models since the fleet average emission factor in ECLIPSE
is 69 % higher than that of MIX, i.e., 9.3 <inline-formula><mml:math id="M211" display="inline"><mml:mrow><mml:mi mathvariant="normal">g</mml:mi><mml:mspace linebreak="nobreak" width="0.125em"/><mml:msup><mml:mi mathvariant="normal">kg</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>
vs. 5.5 <inline-formula><mml:math id="M212" display="inline"><mml:mrow><mml:mi mathvariant="normal">g</mml:mi><mml:mspace linebreak="nobreak" width="0.125em"/><mml:msup><mml:mi mathvariant="normal">kg</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>.</p>
      <p id="d1e4105"><italic>Diesel</italic>. As shown in Table 3, the significant diesel emission
discrepancies can be primarily attributed to the differences in fuel
consumption. Compared to MIX, ECLIPSE has 22 % lower diesel use
for on-road vehicles and 39 % lower for off-road engines. While
applied emission factors are comparable for most categories, there is a
large discrepancy for light-duty vehicles, where the MIX value is 4
times larger than ECLIPSE. One possible explanation is that there
might be an issue with assumptions about fuel efficiency that were
applied when converting the native MEIC values, which are kilometers
driven for activity and gram per kilometer for emission factors (Zheng
et al., 2014).</p>
</sec>
<sec id="Ch1.S3.SS1.SSS2">
  <title>Provincial emission estimates</title>
      <p id="d1e4116">Provincial emissions were developed using different methodologies for two
inventories (see Sect. 2.1). The provincial emission discrepancies
between two inventories are attributed primarily to two factors:
(i) the differences in activities, emission factors and policy
implementation assumptions at the national level (as discussed in the
previous section) and (ii) distribution of activities among the
provinces – see Sect. 2.1 for principal data sources for the latter.</p>
      <p id="d1e4119">Figure 2 compares emissions and the relative difference in fossil fuel
consumption by province in ECLIPSE and MIX in 2010. The differences in
provincial <inline-formula><mml:math id="M213" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> emissions are relatively large for a number of
provinces, especially when compared to the fluctuations of coal
consumption.  This indicates significant differences in provincial
emission factors, which is mainly because of varying assumptions on
application and efficiency of abatement measures but also different
allocation of coal use between power and industry since emission
standards for these sectors are different. MIX estimates lower
emissions mainly for eastern China, including Shandong, Hebei, Henan,
Jiangsu, Sichuan, Zhejiang and Anhui.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F2" specific-use="star"><caption><p id="d1e4135">Comparisons of emission estimates and fuel consumption by
province in China in 2010. Values out of <inline-formula><mml:math id="M214" display="inline"><mml:mi>y</mml:mi></mml:math></inline-formula> axis range are labeled
separately in the graphs. Abbreviations of provinces are provided in
Table S3.</p></caption>
            <?xmltex \igopts{width=369.885827pt}?><graphic xlink:href="https://acp.copernicus.org/articles/18/3433/2018/acp-18-3433-2018-f02.png"/>

          </fig>

      <p id="d1e4151">For <inline-formula><mml:math id="M215" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>, ECLIPSE estimates are systematically lower than
MIX for most provinces. For 20 provinces, mainly located in
northern and central China, such as Hebei, Shanxi, Inner Mongolia,
Liaoning, Jilin, Heilongjiang and Shandong, ECLIPSE emissions are
lower by over 20 %. For Beijing, however, ECLIPSE
emissions are 41 % higher than MIX driven by a larger estimate for
power plants (<inline-formula><mml:math id="M216" display="inline"><mml:mo>+</mml:mo></mml:math></inline-formula>36 %) and transport (<inline-formula><mml:math id="M217" display="inline"><mml:mo>+</mml:mo></mml:math></inline-formula>114 %). In general,
assumptions about diesel consumption in transport vary significantly
between inventories, highlighting the need for further validation of
the regional fuel statistics. It is important to note that, as in many
other countries, the national and regional energy use statistics
contain limited information about diesel fuel use in trucks and
non-road engines used in industries in which fuels are allocated to the
industry rather than the transport.</p>
      <p id="d1e4180">The sectorial distributions of emissions by province are generally
consistent between the two inventories, as presented in Fig. S1 in the Supplement. For
<inline-formula><mml:math id="M218" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>, the emission fractions of power plants in MIX are lower,
and industrial fractions are overall higher than those of ECLIPSE due
to the differences in source classification and emission factors. The
distribution patterns of <inline-formula><mml:math id="M219" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> provincial emissions show
relatively good consistency (within 30 % difference on the sector
level) between the two inventories.</p>
</sec>
<sec id="Ch1.S3.SS1.SSS3">
  <title>Gridded emissions</title>
      <p id="d1e4211">Gridded emissions are direct inputs for atmospheric chemistry models
and climate models. We compared ECLIPSE and MIX gridded emissions by
analyzing three components: emissions by grids at <inline-formula><mml:math id="M220" display="inline"><mml:mrow><mml:mn mathvariant="normal">0.5</mml:mn><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup><mml:mo>×</mml:mo><mml:mn mathvariant="normal">0.5</mml:mn><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:mrow></mml:math></inline-formula> resolution in 2010, the spatial proxies used in the gridding
process and gridded emission trends from 2005 to 2010.</p>
      <p id="d1e4234"><italic>Gridded emissions</italic>. Figure 3 compares the gridded emissions between
ECLIPSE and MIX for <inline-formula><mml:math id="M221" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> and <inline-formula><mml:math id="M222" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>. MIX emissions were
aggregated from 0.25 to 0.5<inline-formula><mml:math id="M223" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> to be comparable with ECLIPSE. The
discrepancies in spatial distribution of gridded emissions are in line with
provincial emission differences discussed earlier. Grids located in eastern
parts of China show higher <inline-formula><mml:math id="M224" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> emissions in ECLIPSE compared to MIX.
<inline-formula><mml:math id="M225" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> emissions of ECLIPSE are overall lower than MIX, except for
Beijing and Guangzhou. Correlations between the two gridded emissions are
quite good at <inline-formula><mml:math id="M226" display="inline"><mml:mrow><mml:mn mathvariant="normal">0.5</mml:mn><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup><mml:mo>×</mml:mo><mml:mn mathvariant="normal">0.5</mml:mn><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:mrow></mml:math></inline-formula> grids (slope <inline-formula><mml:math id="M227" display="inline"><mml:mrow><mml:mo>=</mml:mo><mml:mn mathvariant="normal">0.83</mml:mn></mml:mrow></mml:math></inline-formula>,
<inline-formula><mml:math id="M228" display="inline"><mml:mrow><mml:mi>R</mml:mi><mml:mo>=</mml:mo><mml:mn mathvariant="normal">0.90</mml:mn></mml:mrow></mml:math></inline-formula> for <inline-formula><mml:math id="M229" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>, slope <inline-formula><mml:math id="M230" display="inline"><mml:mrow><mml:mo>=</mml:mo><mml:mn mathvariant="normal">0.79</mml:mn></mml:mrow></mml:math></inline-formula>, <inline-formula><mml:math id="M231" display="inline"><mml:mrow><mml:mi>R</mml:mi><mml:mo>=</mml:mo><mml:mn mathvariant="normal">0.98</mml:mn></mml:mrow></mml:math></inline-formula> for <inline-formula><mml:math id="M232" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>).</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F3" specific-use="star"><caption><p id="d1e4382">Comparisons of MIX and ECLIPSE gridded emissions on
<inline-formula><mml:math id="M233" display="inline"><mml:mrow><mml:mn mathvariant="normal">0.5</mml:mn><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup><mml:mo>×</mml:mo><mml:mn mathvariant="normal">0.5</mml:mn><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:mrow></mml:math></inline-formula> grids for 2010.</p></caption>
            <?xmltex \igopts{width=497.923228pt}?><graphic xlink:href="https://acp.copernicus.org/articles/18/3433/2018/acp-18-3433-2018-f03.png"/>

          </fig>

      <p id="d1e4411">Sectorial emissions show distinct spatial characteristics (Fig. 3b).
Comparisons of industrial and residential sectors show clear
administrative boundaries as these are typically distributed from
provincial emissions using population-based proxies. Since power
plants are treated as point sources, emissions differ in grids over
the entire country, higher for <inline-formula><mml:math id="M234" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> and lower for
<inline-formula><mml:math id="M235" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> in ECLIPSE. Signals of large cities are observed in
the comparison for the transportation sector because emissions are gridded
based on road network (on-road) or population distribution (off-road).</p>
      <p id="d1e4437">The differences of gridded emissions illustrated in Fig. 3 are
attributed to the discrepancies in emission estimates nationwide and
by provinces (Sect. 3.1.1, 3.1.2) and also method and data of
emission spatial allocations (see Sect. 2). For power plants that
were treated as point sources, emissions are gridded based on the
locations verified by Google Earth (Liu et al., 2015), consistent
between ECLIPSE and MIX. For other sectors, ECLIPSE gridded the
provincial emissions according to the source-specific layers, and MEIC
used a two-step allocation method (province to county, county to
grid). The data sources of spatial proxies also differ between the two
inventories (see Table S1). We further compared the spatial proxies by
sector in Fig. 4.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F4" specific-use="star"><caption><p id="d1e4442">Emission distribution ratios within provinces in China in
2010 at <inline-formula><mml:math id="M236" display="inline"><mml:mrow><mml:mn mathvariant="normal">0.5</mml:mn><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup><mml:mo>×</mml:mo><mml:mn mathvariant="normal">0.5</mml:mn><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:mrow></mml:math></inline-formula> resolution.</p></caption>
            <?xmltex \igopts{width=497.923228pt}?><graphic xlink:href="https://acp.copernicus.org/articles/18/3433/2018/acp-18-3433-2018-f04.png"/>

          </fig>

      <p id="d1e4471"><italic>Spatial proxy</italic>. Spatial proxies can play key roles in
evaluating the accuracy of emission inventories and CTM simulation (Geng
et al., 2017; Zheng et al., 2017).  Proxies used in the ECLIPSE and MIX
emission gridding process are summarized in Sect. 2. Source-specific
layers were developed as spatial proxies by ECLIPSE, among which, MEIC
emissions were taken to distribute emissions for power plants (Klimont
et al., 2017). For the industry and residential sectors, emissions are
distributed mainly based on population data. Road networks and
population are used as proxies for transportation emissions. The spatial
proxies used in MIX (MEIC) have been summarized in several papers
(Geng et al., 2017; Li et al., 2017), showing that local proxies are
used in the gridding process. MIX (MEIC) uses Google Earth in verifying
the locations for each power plant. As described in Zheng
et al. (2014), for the transport sector, the China digital
road-network map is used for emission distribution. Other proxies
including the total population map (for some industrial sources),
urban population map (for industrial heating, residential coal
burning, etc.) and rural population map (for residential biofuel
burning) are in general consistent with the global inventory (Geng
et al., 2017).</p>
      <p id="d1e4476">In this work, we calculated the distribution ratios, reflecting the
spatial proxies used, by dividing the emissions for each grid by the
provincial emissions for each sector. The distribution ratios between
ECLIPSE and MIX in 2010 are shown in Fig. 4. Good correlations
(slope <inline-formula><mml:math id="M237" display="inline"><mml:mrow><mml:mo>≥</mml:mo><mml:mn mathvariant="normal">0.79</mml:mn></mml:mrow></mml:math></inline-formula>, <inline-formula><mml:math id="M238" display="inline"><mml:mrow><mml:mi>R</mml:mi><mml:mo>≥</mml:mo><mml:mn mathvariant="normal">0.94</mml:mn></mml:mrow></mml:math></inline-formula>) are observed for all sectors, which
is reasonable because similar proxy datasets were used in the two
inventories, as illustrated above. The differences for specific
sectors (e.g., residential with a slope of 0.87, transportation with a
slope of 0.79–0.81) are higher than others, mainly due to the
different population datasets and road networks used for emission
allocation of relevant sources in ECLIPSE and MIX.</p>
      <p id="d1e4501"><italic>Emission trend (2005</italic>–<italic>2010)</italic>. Fig. 5 presents the emission changes
of <inline-formula><mml:math id="M239" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> and <inline-formula><mml:math id="M240" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> estimated by ECLIPSE and MIX for the
period of 2005 to 2010. For <inline-formula><mml:math id="M241" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>, the emission trends are similar
between the two inventories: a sharp decrease for power plants due to the
wide application of desulfurization facilities since 2006 and an overall
increase for industrial sources driven by economic growth and still low
penetration of emission control technology, consistent with the national
emission trend analyses in Sect. 3.1.1. For <inline-formula><mml:math id="M242" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>, different
emission trends are estimated for transportation and consistent trends are
estimated for other sectors.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F5" specific-use="star"><caption><p id="d1e4556"><inline-formula><mml:math id="M243" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> <bold>(a)</bold> and <inline-formula><mml:math id="M244" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> <bold>(b)</bold>
emission changes from 2005 to 2010 by sectors calculated as
<inline-formula><mml:math id="M245" display="inline"><mml:mrow><mml:msub><mml:mi>E</mml:mi><mml:mn mathvariant="normal">2010</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>–<inline-formula><mml:math id="M246" display="inline"><mml:mrow><mml:msub><mml:mi>E</mml:mi><mml:mn mathvariant="normal">2005</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>, at <inline-formula><mml:math id="M247" display="inline"><mml:mrow><mml:mn mathvariant="normal">0.5</mml:mn><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup><mml:mo>×</mml:mo><mml:mn mathvariant="normal">0.5</mml:mn><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:mrow></mml:math></inline-formula>
grids. Note different color scales are used among sectors.</p></caption>
            <?xmltex \igopts{width=497.923228pt}?><graphic xlink:href="https://acp.copernicus.org/articles/18/3433/2018/acp-18-3433-2018-f05.png"/>

          </fig>

      <p id="d1e4635">In MIX, decreasing emissions for the Beijing and PRD (Pearl River Delta)
regions are estimated, which are dominated by a decline in the power and
transport sectors, in contrast to the increasing emission trend of
ECLIPSE. The different trends of transportation emissions are
attributed to the different assumptions about the legislation effect on
pollution control in the two inventory systems. For Beijing, the
differences in the transportation emission trend are mainly caused by
diesel vehicles. In ECLIPSE, 47 % increases are estimated for
diesel-fueled vehicles, compared to 28 % emission decreases in
MIX.  Fuel consumptions show large discrepancies in the trend from 2005 to
2010, with <inline-formula><mml:math id="M248" display="inline"><mml:mo>+</mml:mo></mml:math></inline-formula>54 % (ECLIPSE) compared to <inline-formula><mml:math id="M249" display="inline"><mml:mo>-</mml:mo></mml:math></inline-formula>20 % (MIX) for
heavy-duty vehicles and <inline-formula><mml:math id="M250" display="inline"><mml:mo>+</mml:mo></mml:math></inline-formula>45 % (ECLIPSE) compared to <inline-formula><mml:math id="M251" display="inline"><mml:mo>+</mml:mo></mml:math></inline-formula>3 %
(MIX) for light-duty vehicles. The emission factors of light-duty
vehicles increase by 5 % in ECLIPSE, whereas they decrease by 34 % in
MIX, attributed to the different assumptions about emission control
effects. As a pioneer in pollution control of China, Beijing carried
out a Euro III standard in 2005 and Euro IV standard in 2008 for light-duty vehicles. The Euro IV penetrations in 2010 in Beijing are
assumed to be
around 12 % in ECLIPSE and more than 60 % in MIX, which
might be too optimistic and should be verified with local surveys.</p>
      <p id="d1e4666">For the PRD region, gasoline and heavy-duty diesel vehicles contribute to the
different emission trends. Of the emission changes for light-duty gasoline buses,
a 22 % increase is estimated in ECLIPSE,
compared to 12 % emission reduction in MIX. For heavy-duty diesel
vehicles, the trends in fuel consumption (<inline-formula><mml:math id="M252" display="inline"><mml:mo>+</mml:mo></mml:math></inline-formula>55 % in ECLIPSE, compared to
<inline-formula><mml:math id="M253" display="inline"><mml:mo>-</mml:mo></mml:math></inline-formula>11 % in MIX) and technology distribution (21 % of Euro III in 2010
for ECLIPSE, compared to <inline-formula><mml:math id="M254" display="inline"><mml:mrow><mml:mo>&gt;</mml:mo><mml:mn mathvariant="normal">50</mml:mn></mml:mrow></mml:math></inline-formula> % in MIX) are the main contributors to
the difference. In summary, survey data are urgently needed to validate the
fuel consumption, effect of legislation and trend for diesel vehicles in
pioneering regions such as Beijing and PRD.</p>
</sec>
</sec>
<sec id="Ch1.S3.SS2">
  <title>Evaluations from the satellite perspective</title>
      <p id="d1e4700">In this section, we evaluated the effect of emission inventories on
the accuracy of model simulations through combing GEOS-Chem
Asian-nested modeling and OMI observations (Sect. 3.2.1). Top-down
emissions were developed for both <inline-formula><mml:math id="M255" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> and <inline-formula><mml:math id="M256" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>
(Sect. 3.2.2). Due to the large uncertainties in <inline-formula><mml:math id="M257" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>
retrievals of OMI, we mainly focused on the evaluations for
<inline-formula><mml:math id="M258" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> emission estimates, spatial proxies and emission
trends.</p>
<sec id="Ch1.S3.SS2.SSS1">
  <title>Sensitivity cases for model simulations</title>
      <p id="d1e4752">The main purpose of this subsection is to evaluate the effect of gridded
emissions on model performance and figure out the effect of emission
estimates and spatial distributions on model performance using satellite
observations as a criterion. Therefore, we set up four sensitivity cases of
modeling, ECL-case0, ECL-case1, ECL-case2 and MIX. ECL-case0 and MIX form the
two basic cases, which apply the ECLIPSE and MIX emissions in the simulation,
respectively. ECL-case1 scales China's emissions in ECLIPSE to MIX's value by
sectors retaining original spatial distributions. ECL-case2 redistributes the
ECLIPSE emissions over China based on the spatial grid ratios of MIX, also on
the sector level. The characteristics of the emission inventory used for each
case are summarized in Table 4 and shown in Fig. S2. We processed each
inventory into model-ready inputs through regridding new emissions,
performing VOC speciation and temporal allocation. The speciation factor and
monthly profiles by sector of the MIX inventory are used for
ECL-case0–case2.
We resample the model results based on satellite observations spatially and
temporally for consistent comparison as described in Sect. 2.3.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F6" specific-use="star"><caption><p id="d1e4757"><inline-formula><mml:math id="M259" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> columns simulated by GEOS-Chem in sensitivity
cases, compared to OMI observations; summer average
(June–July–August) in 2010. Unit: 1 DU <inline-formula><mml:math id="M260" display="inline"><mml:mrow><mml:mo>=</mml:mo><mml:mn mathvariant="normal">2.69</mml:mn><mml:mo>×</mml:mo><mml:msup><mml:mn mathvariant="normal">10</mml:mn><mml:mn mathvariant="normal">16</mml:mn></mml:msup></mml:mrow></mml:math></inline-formula>  <inline-formula><mml:math id="M261" display="inline"><mml:mrow><mml:mi mathvariant="normal">molec</mml:mi><mml:mspace width="0.125em" linebreak="nobreak"/><mml:msup><mml:mi mathvariant="normal">cm</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">2</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>.</p></caption>
            <?xmltex \igopts{width=341.433071pt}?><graphic xlink:href="https://acp.copernicus.org/articles/18/3433/2018/acp-18-3433-2018-f06.png"/>

          </fig>

<?xmltex \floatpos{t}?><table-wrap id="Ch1.T4" specific-use="star"><caption><p id="d1e4813">Description of model simulation cases and statistics of
model performance of <inline-formula><mml:math id="M262" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>; summer average in 2010.</p></caption><oasis:table frame="topbot"><oasis:tgroup cols="7">
     <oasis:colspec colnum="1" colname="col1" align="left"/>
     <oasis:colspec colnum="2" colname="col2" align="left"/>
     <oasis:colspec colnum="3" colname="col3" align="left"/>
     <oasis:colspec colnum="4" colname="col4" align="right"/>
     <oasis:colspec colnum="5" colname="col5" align="right"/>
     <oasis:colspec colnum="6" colname="col6" align="right"/>
     <oasis:colspec colnum="7" colname="col7" align="right"/>
     <oasis:thead>
       <oasis:row>  
         <oasis:entry colname="col1">Simulation</oasis:entry>  
         <oasis:entry colname="col2">Emission</oasis:entry>  
         <oasis:entry colname="col3">Spatial</oasis:entry>  
         <oasis:entry colname="col4"><inline-formula><mml:math id="M269" display="inline"><mml:mi>R</mml:mi></mml:math></inline-formula></oasis:entry>  
         <oasis:entry colname="col5">Slope</oasis:entry>  
         <oasis:entry colname="col6">NMB<inline-formula><mml:math id="M270" display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">a</mml:mi></mml:msup></mml:math></inline-formula></oasis:entry>  
         <oasis:entry colname="col7">RMSE<inline-formula><mml:math id="M271" display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">b</mml:mi></mml:msup></mml:math></inline-formula></oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1">cases</oasis:entry>  
         <oasis:entry colname="col2">estimates</oasis:entry>  
         <oasis:entry colname="col3">proxies</oasis:entry>  
         <oasis:entry colname="col4"/>  
         <oasis:entry colname="col5"/>  
         <oasis:entry colname="col6">(%)</oasis:entry>  
         <oasis:entry colname="col7">(10<inline-formula><mml:math id="M272" display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">15</mml:mn></mml:msup></mml:math></inline-formula> mol</oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">  
         <oasis:entry colname="col1"/>  
         <oasis:entry colname="col2"/>  
         <oasis:entry colname="col3"/>  
         <oasis:entry colname="col4"/>  
         <oasis:entry colname="col5"/>  
         <oasis:entry colname="col6"/>  
         <oasis:entry colname="col7">cm<inline-formula><mml:math id="M273" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">2</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula>)</oasis:entry>
       </oasis:row>
     </oasis:thead>
     <oasis:tbody>
       <oasis:row>  
         <oasis:entry colname="col1">ECL-case0</oasis:entry>  
         <oasis:entry colname="col2">EM-ECL<inline-formula><mml:math id="M274" display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">c</mml:mi></mml:msup></mml:math></inline-formula></oasis:entry>  
         <oasis:entry colname="col3">SP-ECL<inline-formula><mml:math id="M275" display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">d</mml:mi></mml:msup></mml:math></inline-formula></oasis:entry>  
         <oasis:entry colname="col4">0.814</oasis:entry>  
         <oasis:entry colname="col5">0.476</oasis:entry>  
         <oasis:entry colname="col6"><inline-formula><mml:math id="M276" display="inline"><mml:mo>-</mml:mo></mml:math></inline-formula>12.2</oasis:entry>  
         <oasis:entry colname="col7">1.19</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1">ECL-case1</oasis:entry>  
         <oasis:entry colname="col2">EM-MIX<inline-formula><mml:math id="M277" display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">e</mml:mi></mml:msup></mml:math></inline-formula></oasis:entry>  
         <oasis:entry colname="col3">SP-ECL</oasis:entry>  
         <oasis:entry colname="col4">0.818</oasis:entry>  
         <oasis:entry colname="col5">0.559</oasis:entry>  
         <oasis:entry colname="col6"><inline-formula><mml:math id="M278" display="inline"><mml:mo>-</mml:mo></mml:math></inline-formula>6.19</oasis:entry>  
         <oasis:entry colname="col7">1.15</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1">ECL-case2</oasis:entry>  
         <oasis:entry colname="col2">EM-ECL</oasis:entry>  
         <oasis:entry colname="col3">SP-MIX<inline-formula><mml:math id="M279" display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">f</mml:mi></mml:msup></mml:math></inline-formula></oasis:entry>  
         <oasis:entry colname="col4">0.824</oasis:entry>  
         <oasis:entry colname="col5">0.474</oasis:entry>  
         <oasis:entry colname="col6"><inline-formula><mml:math id="M280" display="inline"><mml:mo>-</mml:mo></mml:math></inline-formula>12.1</oasis:entry>  
         <oasis:entry colname="col7">1.18</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1">MIX</oasis:entry>  
         <oasis:entry colname="col2">EM-MIX</oasis:entry>  
         <oasis:entry colname="col3">SP-MIX</oasis:entry>  
         <oasis:entry colname="col4">0.811</oasis:entry>  
         <oasis:entry colname="col5">0.601</oasis:entry>  
         <oasis:entry colname="col6"><inline-formula><mml:math id="M281" display="inline"><mml:mo>-</mml:mo></mml:math></inline-formula>4.72</oasis:entry>  
         <oasis:entry colname="col7">1.16</oasis:entry>
       </oasis:row>
     </oasis:tbody>
   </oasis:tgroup></oasis:table><table-wrap-foot><p id="d1e4827"><inline-formula><mml:math id="M263" display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">a</mml:mi></mml:msup></mml:math></inline-formula> Normalized Mean Bias.<?xmltex \hack{\\}?><inline-formula><mml:math id="M264" display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">b</mml:mi></mml:msup></mml:math></inline-formula> Root Mean Square Error.<?xmltex \hack{\\}?><inline-formula><mml:math id="M265" display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">c</mml:mi></mml:msup></mml:math></inline-formula> ECLIPSE emission estimates by sector in China.<?xmltex \hack{\\}?><inline-formula><mml:math id="M266" display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">d</mml:mi></mml:msup></mml:math></inline-formula> Spatial proxies by sector based on ECLIPSE.<?xmltex \hack{\\}?><inline-formula><mml:math id="M267" display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">e</mml:mi></mml:msup></mml:math></inline-formula> MIX emission estimates by sector in China.<?xmltex \hack{\\}?><inline-formula><mml:math id="M268" display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">f</mml:mi></mml:msup></mml:math></inline-formula> Spatial proxies by sector based on MIX. </p></table-wrap-foot></table-wrap>

      <p id="d1e5181">Figure 6 compares the <inline-formula><mml:math id="M282" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> columns simulated by the four model
cases and OMI <inline-formula><mml:math id="M283" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> columns in 2010. Although OMI data tend to
overestimate the concentrations due to the overlap in signals of
<inline-formula><mml:math id="M284" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> and <inline-formula><mml:math id="M285" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> during retrieval, good correlations are
found between model results and satellite observations (<inline-formula><mml:math id="M286" display="inline"><mml:mrow><mml:mi>R</mml:mi><mml:mo>=</mml:mo><mml:mn mathvariant="normal">0.633</mml:mn></mml:mrow></mml:math></inline-formula>–0.667,
slope <inline-formula><mml:math id="M287" display="inline"><mml:mrow><mml:mo>=</mml:mo><mml:mn mathvariant="normal">0.842</mml:mn></mml:mrow></mml:math></inline-formula>–0.863, generally consistent among sensitivity cases;
see Table S4), confirming the high accuracies of the priori
<inline-formula><mml:math id="M288" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> spatial emission patterns.</p>
      <p id="d1e5262"><inline-formula><mml:math id="M289" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">NO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> tropospheric vertical columns modeled for each case are
compared with the retrieved OMI columns (Fig. 7). Summer-averaged
results are shown here because of the closer connection between
emissions and columns due to short <inline-formula><mml:math id="M290" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> lifetime. As shown
in Fig. 7, a modeled <inline-formula><mml:math id="M291" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">NO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> density map shows a similar spatial
pattern among cases, but different magnitudes. Higher <inline-formula><mml:math id="M292" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">NO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>
concentrations are observed for the ECL-case1 and MIX case because
common emission estimates of MIX are used, which are higher than
ECLIPSE.  Compared to OMI, all model cases underestimate the pollution
in northern China and slightly overestimate the columns over central
China. As illustrated in Table 4, the performance of the MIX case is the
best among all cases, identified by low biases (<inline-formula><mml:math id="M293" display="inline"><mml:mrow><mml:mtext>NMB</mml:mtext><mml:mo>=</mml:mo><mml:mo>-</mml:mo><mml:mn mathvariant="normal">4.72</mml:mn></mml:mrow></mml:math></inline-formula> %) and a better slope ratio (slope <inline-formula><mml:math id="M294" display="inline"><mml:mrow><mml:mo>=</mml:mo><mml:mn mathvariant="normal">0.601</mml:mn></mml:mrow></mml:math></inline-formula>). The results of
ECL-case0 and ECL-case2 are similar because the differences in spatial
proxies of two inventories are small compared to the differences in
emission estimates (Sect. 3.1.3). Replacing the emission estimates of
ECLIPSE with MIX improves the model performance from bias at <inline-formula><mml:math id="M295" display="inline"><mml:mo>-</mml:mo></mml:math></inline-formula>12.2
to <inline-formula><mml:math id="M296" display="inline"><mml:mo>-</mml:mo></mml:math></inline-formula>6.19 % (ECL-case1 vs. ECL-case0).</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F7" specific-use="star"><caption><p id="d1e5349"><inline-formula><mml:math id="M297" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">NO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> tropospheric columns simulated by GEOS-Chem in
sensitivity cases. For each case, the specific <inline-formula><mml:math id="M298" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">NO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> vertical
profiles were applied in inversion; summer average
(June–July–August) in 2010.</p></caption>
            <?xmltex \igopts{width=312.980315pt}?><graphic xlink:href="https://acp.copernicus.org/articles/18/3433/2018/acp-18-3433-2018-f07.png"/>

          </fig>

</sec>
<sec id="Ch1.S3.SS2.SSS2">
  <title>Top-down emission evaluations</title>
      <p id="d1e5385">Satellite-based emission inventories were developed following the
finite difference mass balance methodology (Cooper et al.,
2017). Emissions of <inline-formula><mml:math id="M299" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> estimated by bottom-up and top-down
inventories are presented in Table S5. Both ECLIPSE and MIX correlate
well with the top-down estimates (<inline-formula><mml:math id="M300" display="inline"><mml:mrow><mml:mi>R</mml:mi><mml:mo>=</mml:mo><mml:mn mathvariant="normal">0.722</mml:mn></mml:mrow></mml:math></inline-formula>–0.896,
slope <inline-formula><mml:math id="M301" display="inline"><mml:mrow><mml:mo>=</mml:mo><mml:mn mathvariant="normal">0.539</mml:mn></mml:mrow></mml:math></inline-formula>–0.923) in 2005 and 2010. Relatively high negative
biases are found (<inline-formula><mml:math id="M302" display="inline"><mml:mrow><mml:mtext>NMB</mml:mtext><mml:mo>=</mml:mo><mml:mo>-</mml:mo><mml:mn mathvariant="normal">51.0</mml:mn><mml:mo>∼</mml:mo><mml:mo>-</mml:mo><mml:mn mathvariant="normal">29.1</mml:mn></mml:mrow></mml:math></inline-formula> %) in
the bottom-up inventories, possibly attributed to the uncertainties in the
OMI retrievals for <inline-formula><mml:math id="M303" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>. Table 5 shows the <inline-formula><mml:math id="M304" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>
emission estimates and correlations between bottom-up and top-down
inventories. For <inline-formula><mml:math id="M305" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>, it can be concluded that ECLIPSE and
MIX are consistent with the top-down estimates over China. Summer-averaged bottom-up emissions show strong correlations with the
top-down ones (<inline-formula><mml:math id="M306" display="inline"><mml:mrow><mml:mi>R</mml:mi><mml:mo>&gt;</mml:mo><mml:mn mathvariant="normal">0.87</mml:mn></mml:mrow></mml:math></inline-formula> for both inventories) in 2010. The mean
biases of MIX are <inline-formula><mml:math id="M307" display="inline"><mml:mo>-</mml:mo></mml:math></inline-formula>21.2 % (11.9 <inline-formula><mml:math id="M308" display="inline"><mml:mrow><mml:mi mathvariant="normal">mol</mml:mi><mml:mspace linebreak="nobreak" width="0.125em"/><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula> in RMSE),
much lower than <inline-formula><mml:math id="M309" display="inline"><mml:mo>-</mml:mo></mml:math></inline-formula>39.4 % of ECLIPSE (14.6 <inline-formula><mml:math id="M310" display="inline"><mml:mrow><mml:mi mathvariant="normal">mol</mml:mi><mml:mspace width="0.125em" linebreak="nobreak"/><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula> in
RMSE). The slope ratio of MIX shows a slightly better performance than
ECLIPSE (0.73 for MIX, 0.50 for ECLIPSE), but should be interpreted
with caution since the slope can be dominated by several large point
sources.</p>

<?xmltex \floatpos{t}?><table-wrap id="Ch1.T5"><caption><p id="d1e5539">Top-down <inline-formula><mml:math id="M311" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> emission evaluations
over China<inline-formula><mml:math id="M312" display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">a</mml:mi></mml:msup></mml:math></inline-formula>.</p></caption><oasis:table frame="topbot"><oasis:tgroup cols="5">
     <oasis:colspec colnum="1" colname="col1" align="justify" colwidth="80pt"/>
     <oasis:colspec colnum="2" colname="col2" align="right"/>
     <oasis:colspec colnum="3" colname="col3" align="right" colsep="1"/>
     <oasis:colspec colnum="4" colname="col4" align="right"/>
     <oasis:colspec colnum="5" colname="col5" align="right"/>
     <oasis:thead>
       <oasis:row rowsep="1">  
         <oasis:entry colname="col1">Inventories</oasis:entry>  
         <oasis:entry namest="col2" nameend="col3" align="center" colsep="1">ECLIPSE </oasis:entry>  
         <oasis:entry namest="col4" nameend="col5" align="center">MIX </oasis:entry>
       </oasis:row>
     </oasis:thead>
     <oasis:tbody>
       <oasis:row>  
         <oasis:entry colname="col1">Year</oasis:entry>  
         <oasis:entry colname="col2">2005</oasis:entry>  
         <oasis:entry colname="col3">2010</oasis:entry>  
         <oasis:entry colname="col4">2005</oasis:entry>  
         <oasis:entry colname="col5">2010</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1">Bottom-up emissions<?xmltex \hack{\hfill\break}?>(<inline-formula><mml:math id="M314" display="inline"><mml:mrow><mml:mi mathvariant="normal">k</mml:mi><mml:mspace linebreak="nobreak" width="0.125em"/><mml:mi mathvariant="normal">mol</mml:mi><mml:mspace linebreak="nobreak" width="0.125em"/><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>)</oasis:entry>  
         <oasis:entry colname="col2">10.4</oasis:entry>  
         <oasis:entry colname="col3">12.2</oasis:entry>  
         <oasis:entry colname="col4">12.5</oasis:entry>  
         <oasis:entry colname="col5">15.4</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1">Top-down emissions<?xmltex \hack{\hfill\break}?>(<inline-formula><mml:math id="M315" display="inline"><mml:mrow><mml:mi mathvariant="normal">k</mml:mi><mml:mspace width="0.125em" linebreak="nobreak"/><mml:mi mathvariant="normal">mol</mml:mi><mml:mspace linebreak="nobreak" width="0.125em"/><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>)</oasis:entry>  
         <oasis:entry colname="col2">17.0</oasis:entry>  
         <oasis:entry colname="col3">20.2</oasis:entry>  
         <oasis:entry colname="col4">16.0</oasis:entry>  
         <oasis:entry colname="col5">19.6</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1"><inline-formula><mml:math id="M316" display="inline"><mml:mi>R</mml:mi></mml:math></inline-formula></oasis:entry>  
         <oasis:entry colname="col2">0.936</oasis:entry>  
         <oasis:entry colname="col3">0.866</oasis:entry>  
         <oasis:entry colname="col4">0.936</oasis:entry>  
         <oasis:entry colname="col5">0.891</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1">Slope</oasis:entry>  
         <oasis:entry colname="col2">0.598</oasis:entry>  
         <oasis:entry colname="col3">0.500</oasis:entry>  
         <oasis:entry colname="col4">0.821</oasis:entry>  
         <oasis:entry colname="col5">0.726</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1">NMB (%)</oasis:entry>  
         <oasis:entry colname="col2"><inline-formula><mml:math id="M317" display="inline"><mml:mo>-</mml:mo></mml:math></inline-formula>38.6</oasis:entry>  
         <oasis:entry colname="col3"><inline-formula><mml:math id="M318" display="inline"><mml:mo>-</mml:mo></mml:math></inline-formula>39.4</oasis:entry>  
         <oasis:entry colname="col4"><inline-formula><mml:math id="M319" display="inline"><mml:mo>-</mml:mo></mml:math></inline-formula>21.8</oasis:entry>  
         <oasis:entry colname="col5"><inline-formula><mml:math id="M320" display="inline"><mml:mo>-</mml:mo></mml:math></inline-formula>21.2</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1">RMSE (<inline-formula><mml:math id="M321" display="inline"><mml:mrow><mml:mi mathvariant="normal">mol</mml:mi><mml:mspace width="0.125em" linebreak="nobreak"/><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>)</oasis:entry>  
         <oasis:entry colname="col2">9.48</oasis:entry>  
         <oasis:entry colname="col3">14.6</oasis:entry>  
         <oasis:entry colname="col4">7.47</oasis:entry>  
         <oasis:entry colname="col5">11.9</oasis:entry>
       </oasis:row>
     </oasis:tbody>
   </oasis:tgroup></oasis:table><table-wrap-foot><p id="d1e5562"><inline-formula><mml:math id="M313" display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">a</mml:mi></mml:msup></mml:math></inline-formula> Only contain grids covered by OMI pixels filtered
by the criterion described in the text.</p></table-wrap-foot></table-wrap>

      <p id="d1e5824">In spatial distribution, large discrepancies are observed between
bottom-up emission inventories and the top-down ones. For <inline-formula><mml:math id="M322" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>,
bottom-up inventories tend to underestimate emissions in Shandong
Province and several southern provinces such as Guizhou, Jiangxi and
Fujian, which may be attributed to the scattered coal consumption, while
overestimating emissions in the Yangtze River Delta (YRD) region (see Fig. 8). As shown in
Fig. 9, both ECLIPSE and MIX underestimate the <inline-formula><mml:math id="M323" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>
emission strength in northern China and parts of the YRD and PRD regions and overestimate emissions located in large
cities such as Beijing, Shanghai and Wuhan. One important reason for
the latter is associated with the limitations of currently used
spatial proxies. Using population or industry gross domestic
product as a spatial proxy may distribute too much emissions to
provincial capitals or economically developed cities. Through
sensitivity test analyses, it is concluded that treating sources as
point sources can significantly reduce the uncertainties in the emission
gridding process (Geng et al., 2017).</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F8" specific-use="star"><caption><p id="d1e5852">Comparisons among ECLIPSE, MIX and top-down emissions of
<inline-formula><mml:math id="M324" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>; summer average in 2010.</p></caption>
            <?xmltex \igopts{width=341.433071pt}?><graphic xlink:href="https://acp.copernicus.org/articles/18/3433/2018/acp-18-3433-2018-f08.jpg"/>

          </fig>

      <?xmltex \floatpos{t}?><fig id="Ch1.F9" specific-use="star"><caption><p id="d1e5874">Comparisons among ECLIPSE, MIX and top-down emissions of
<inline-formula><mml:math id="M325" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>; summer average in 2010.</p></caption>
            <?xmltex \igopts{width=369.885827pt}?><graphic xlink:href="https://acp.copernicus.org/articles/18/3433/2018/acp-18-3433-2018-f09.jpg"/>

          </fig>

      <p id="d1e5894">Emission changes from 2005 to 2010 were evaluated and presented in
Fig. 10 for <inline-formula><mml:math id="M326" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> and Fig. 11 for <inline-formula><mml:math id="M327" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>. The maps of
<inline-formula><mml:math id="M328" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> emission changes are consistent in spatial patterns
between bottom-up and top-down inventories. Effective control measures
including nationwide FGD application led to a significant <inline-formula><mml:math id="M329" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>
emission decrease between 2005 and 2010, especially in Beijing, Hebei,
Shanxi, YRD, PRD and the southwest provinces of China. The annual growth
rate of China's emissions of <inline-formula><mml:math id="M330" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> is highly consistently
estimated by ECLIPSE, MIX and satellite-based inventories, around
4.0 % annual growth in the period of 2005 to 2010 (see Table 5).
The results are comparable with previous work using various inversion
methodologies, satellite sensors or CTMs (Gu et al., 2013; Krotkov
et al., 2016; Miyazaki et al., 2017). Figure 11 shows the gridded
emission changes from 2005 to 2010 among different inventories for
<inline-formula><mml:math id="M331" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>. A decrease in parts of the YRD and PRD regions and shut down
of large facilities are captured by satellite, showing generally
consistency with MIX. Significantly larger growth is observed in
northern China's emissions from top-down inventories than in
estimates of ECLIPSE and MIX. In Beijing, the satellite-based
inventory shows a relatively stable trend, different from the increasing
trend of ECLIPSE or decreasing trend of MIX, indicating that
assumptions about the penetration of emission reduction technology
need further revision in both inventory models for large cities.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F10" specific-use="star"><caption><p id="d1e5966"><inline-formula><mml:math id="M332" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> emission changes from 2005 to 2010, estimated by
ECLIPSE, MIX and a derived top-down inventory for each case; summer
average (JJA).</p></caption>
            <?xmltex \igopts{width=398.338583pt}?><graphic xlink:href="https://acp.copernicus.org/articles/18/3433/2018/acp-18-3433-2018-f10.jpg"/>

          </fig>

      <?xmltex \floatpos{t}?><fig id="Ch1.F11" specific-use="star"><caption><p id="d1e5988"><inline-formula><mml:math id="M333" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> emission changes from 2005 to 2010, estimated
by ECLIPSE, MIX and derived top-down inventories for each case;
summer average (JJA).</p></caption>
            <?xmltex \igopts{width=398.338583pt}?><graphic xlink:href="https://acp.copernicus.org/articles/18/3433/2018/acp-18-3433-2018-f11.jpg"/>

          </fig>

</sec>
</sec>
<sec id="Ch1.S3.SS3">
  <title>Discussion</title>
<sec id="Ch1.S3.SS3.SSS1">
  <title>Summary of key parameters contributing to emission
uncertainties</title>
      <p id="d1e6019">We address several key factors contributing to the differences between
ECLIPSE and MIX for <inline-formula><mml:math id="M334" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> and <inline-formula><mml:math id="M335" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> emission
estimates: source classification, energy statistics, emission factors,
assumptions about control technology penetration and spatial proxies.</p>
      <p id="d1e6044">The source classification for heating plants, fuel conversion and industrial
boilers is differently defined between ECLIPSE (GAINS model) and MIX (MEIC
model), making the interpretation of comparisons for each source more
difficult and to some degree less transparent (Sect. 3.1.1). The
source-structure
differences are inevitable for emission inventory models designed for
estimates on different spatial scales. As a global inventory model, GAINS
integrates statistics from international sources (e.g., IEA, FAO). Therefore,
the source structure of GAINS is set up in accordance with the international
statistics framework. Focusing on emissions on a regional scale, MEIC set up
a calculation framework based on statistics from local agencies in China to
gain higher specificity in temporal and spatial distribution (e.g., NBS,
CPED). As illustrated and analyzed in Sect. 3.1.1, the differences by sector
should be interpreted with caution, especially for the power and industry
sectors.</p>
      <p id="d1e6047">The apparent emission uncertainty ratios (the ratio of the maximum
emission discrepancy to the mean value using provincial energy
statistics or national statistics) of <inline-formula><mml:math id="M336" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> and <inline-formula><mml:math id="M337" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>
resulting from energy use are 30 and 16 % according to Hong
et al. (2017). For <inline-formula><mml:math id="M338" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>, emission uncertainties are quite
sensitive to the energy use uncertainty mostly contributed by
industrial coal use (Hong et al., 2017). Based on this work, diesel
consumption in the transport sector remains highly uncertain, contributing
to the emission differences for <inline-formula><mml:math id="M339" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>.</p>
      <p id="d1e6094">The FGD penetration rate in power plants, as well as assumed removal
efficiencies, significantly affect the <inline-formula><mml:math id="M340" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> emission estimates
and trends. Similarly, for <inline-formula><mml:math id="M341" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>, application rates and
abatement efficiency of LNB technology installed in power plants is
significantly different in the models compared; these assumptions
should be further verified and constrained. Emission factors for
diverse industrial boiler types are the main contributors to the
uncertainty in the industrial emissions.  Assumptions about vehicle
fleet, implementation of emission standards and emission factors for
various vehicle types still differ among the investigated inventory
models. More in situ measurements and local surveys are needed to
reduce these uncertainties.</p>
      <p id="d1e6120">Spatial proxies used in emission inventories are an important factor
contributing to the overall accuracy in model simulation. Integration
of detailed spatial information that is often included in regional
inventories like MIX should be considered as the best way to improve
the resolution and spatial allocation of emissions in global products
like ECLIPSE.</p>
</sec>
<sec id="Ch1.S3.SS3.SSS2">
  <title>Uncertainty of top-down evaluation</title>
      <p id="d1e6129">In this work, moderate negative biases are observed in bottom-up
emission inventories (<inline-formula><mml:math id="M342" display="inline"><mml:mo>-</mml:mo></mml:math></inline-formula>21 % for MIX, <inline-formula><mml:math id="M343" display="inline"><mml:mo>-</mml:mo></mml:math></inline-formula>39 % for ECLIPSE),
compared to satellite-based ones. But the top-down evaluations are
subject to uncertainties from both satellite retrievals and model
simulations. The uncertainties of retrieved individual <inline-formula><mml:math id="M344" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">NO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>
columns of the DOMINO v2.0 product are estimated at <inline-formula><mml:math id="M345" display="inline"><mml:mrow><mml:mn mathvariant="normal">1.0</mml:mn><mml:mo>×</mml:mo><mml:msup><mml:mn mathvariant="normal">10</mml:mn><mml:mn mathvariant="normal">15</mml:mn></mml:msup></mml:mrow></mml:math></inline-formula> molecules <inline-formula><mml:math id="M346" display="inline"><mml:mrow><mml:msup><mml:mi mathvariant="normal">cm</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msup></mml:mrow></mml:math></inline-formula>, <inline-formula><mml:math id="M347" display="inline"><mml:mo>+</mml:mo></mml:math></inline-formula>25 % mainly arising from the
AMF calculation (Boersma et al., 2007, 2011).  Because of the high
aerosol loadings in eastern China, the aerosol scattering and
absorption have positive or negative effects on <inline-formula><mml:math id="M348" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">NO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> retrieval,
with a mean effect of 14 % (Lin et al., 2014). A negative systematic
bias of 10–20 % by season plus a random error of 30 % are
generated by model simulation using GEOS-Chem (Martin et al., 2003;
Lin and McElroy, 2010; Lin, 2012). As suggested by Ding et al. (2017),
multiple sensors can give more comprehensive and accurate constraints
on the priori spatial and temporal emission estimates, which can be
further applied in future work.</p>
</sec>
</sec>
</sec>
<sec id="Ch1.S4" sec-type="conclusions">
  <title>Concluding remarks</title>
      <p id="d1e6210">We conducted parameter-level comparisons of gridded Chinese emissions
between ECLIPSE and MIX, elucidated the effect on CTM simulations, and
evaluated the inventories based on OMI observations. This work is
important for inventory developers and modelers for understanding the
potential uncertainties in the gridded emission inventory over
China. For inventory developers, the detailed comparisons give
indications on the underlying uncertainties of parameters by source,
including the source classifications, activity rates, emission factors
and technology distributions. For modelers, the comparisons and
validations are important to understand the effect of emissions on
model performance. This work shows that our best inventories appear to
be fit for evaluation of the policies at an aggregated or national
level; more work is needed in specific areas in order to improve
accuracy and robustness of outcomes at the finer spatial and also
technological levels. The main findings are as follows.
<list list-type="custom"><list-item><label>(a)</label><p id="d1e6214">In 2010, compared to MIX, the emission estimates of ECLIPSE
are identical for <inline-formula><mml:math id="M349" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> and 16 % lower for
<inline-formula><mml:math id="M350" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>. <inline-formula><mml:math id="M351" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> emissions of power plants and industry
sectors differ by <inline-formula><mml:math id="M352" display="inline"><mml:mo>+</mml:mo></mml:math></inline-formula>40 and <inline-formula><mml:math id="M353" display="inline"><mml:mo>-</mml:mo></mml:math></inline-formula>24 % (ECLIPSE compared to MIX),
attributed to the differences in source classification system, FGD
penetration rates and assumed removal efficiencies. Emission
factors for diverse industrial boiler types are the main reason for
the industrial emission differences. For <inline-formula><mml:math id="M354" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>, ECLIPSE
estimates are lower than those of MIX for all sectors. Lower
<inline-formula><mml:math id="M355" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> emission factors for power plants and lower diesel
consumptions in the transport sector in ECLIPSE are the main reasons
for the discrepancies. Application rates and abatement efficiency of
plants equipped with LNBs should be further verified and
constrained. Assumptions about vehicle fleet, implementation of
emission standards and emission factors for various vehicle types
still differ between evaluated inventory models. Large uncertainties
should be addressed for the diesel consumptions in current inventory
models.</p></list-item><list-item><label>(b)</label><p id="d1e6287">We modeled four sensitivity cases to investigate the effect
of emission estimates and spatial proxies of emission inventories on
model accuracy using GEOS-Chem. The model case using MIX as input
shows the best performance, with mean biases at <inline-formula><mml:math id="M356" display="inline"><mml:mo>-</mml:mo></mml:math></inline-formula>4.72 % (NMB,
for <inline-formula><mml:math id="M357" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>). Increasing the ECLIPSE emission estimates to
MIX levels reduces the biases from <inline-formula><mml:math id="M358" display="inline"><mml:mo>-</mml:mo></mml:math></inline-formula>12.2 to <inline-formula><mml:math id="M359" display="inline"><mml:mo>-</mml:mo></mml:math></inline-formula>6.19 % (for
<inline-formula><mml:math id="M360" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>). For ECLIPSE, changing the spatial pattern to that of MIX apparently does
not affect the model results, owing to the role the power
sector (ECLIPSE uses MEIC proxy already) plays in
emissions. Top-down emissions were developed based on OMI
retrievals. High correlations were observed between the bottom-up
and top-down <inline-formula><mml:math id="M361" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> emissions, providing evidence of the
accuracy of the spatial emission patterns in ECLIPSE and MIX. We
found moderate negative biases in bottom-up emission inventories for
<inline-formula><mml:math id="M362" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> (<inline-formula><mml:math id="M363" display="inline"><mml:mo>-</mml:mo></mml:math></inline-formula>21 % for MIX, <inline-formula><mml:math id="M364" display="inline"><mml:mo>-</mml:mo></mml:math></inline-formula>39 % for ECLIPSE),
compared to satellite-based ones.</p></list-item><list-item><label>(c)</label><p id="d1e6370">Both inventories show decreasing trends for <inline-formula><mml:math id="M365" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> and
increasing trends for <inline-formula><mml:math id="M366" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> between 2005 and 2010 but the
spatial pattern of change differs. Signals of large power plants and
of city centers can be found.  Trend analyses from the top-down
perspective indicate an annual growth rate of 4 % for
<inline-formula><mml:math id="M367" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>, consistent with development of bottom-up emissions.
A strong <inline-formula><mml:math id="M368" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> emission increase in northern China and
decrease in parts of the YRD and PRD regions are captured by the
satellite retrievals, similar to the MIX estimates.</p></list-item></list></p>
</sec>

      
      </body>
    <back><notes notes-type="dataavailability">

      <p id="d1e6422">ECLIPSE v5a global emissions developed based on the
GAINS model can be publicly accessed from
<uri>http://www.iiasa.ac.at/web/home/research/researchPrograms/air/ECLIPSEv5a.html</uri>.
The specific parameters of the GAINS model were retrieved from <uri>http://gains.iiasa.ac.at/models/</uri>.  The MIX inventory is publicly
available from <uri>http://www.meicmodel.org/dataset-mix.html</uri>.
China's emissions in MIX are obtained from MEIC v1.2, which is
downloaded from <uri>http://www.meicmodel.org/index.html</uri>. The L2
swath <inline-formula><mml:math id="M369" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> column data developed by NASA are available at
<uri>https://disc.gsfc.nasa.gov/</uri>.  The tropospheric <inline-formula><mml:math id="M370" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">NO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>
column data of DOMINO v2 can be accessed from <uri>www.temis.nl</uri>.</p>
  </notes><app-group>
        <supplementary-material position="anchor"><p id="d1e6466"><bold>The Supplement related to this article is available online at <inline-supplementary-material xlink:href="https://doi.org/10.5194/acp-18-3433-2018-supplement" xlink:title="pdf">https://doi.org/10.5194/acp-18-3433-2018-supplement</inline-supplementary-material>.</bold></p></supplementary-material>
        </app-group><notes notes-type="competinginterests">

      <p id="d1e6472">The authors declare that they have no conflict of
interest.</p>
  </notes><notes notes-type="sistatement">

      <p id="d1e6478">This article is part of the special issue “Global and regional
assessment of intercontinental transport of air pollution: results from HTAP,
AQMEII and MICS”. It is not associated with a conference.</p>
  </notes><ack><title>Acknowledgements</title><p id="d1e6484">This work was supported by the National Key R&amp;D program
(2016YFC0201506), the National Natural Science Foundation of China
(41625020) and IIASA's Young Scientists Summer Program (YSSP)
sponsored by the National Natural Science Foundation of China
(41611140118). We acknowledge the free use of the NASA OMI <inline-formula><mml:math id="M371" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>
and DOMINO v2 products.<?xmltex \hack{\newline}?><?xmltex \hack{\newline}?>
Edited by: Christian Hogrefe<?xmltex \hack{\newline}?>
Reviewed by: two anonymous referees</p></ack><ref-list>
    <title>References</title>

      <ref id="bib1.bib1"><label>1</label><mixed-citation>Amann, M., Bertok, I., Borken-Kleefeld, J., Cofala, J., Heyes, C., Höglund-Isaksson, L., Klimont, Z., Nguyen, B., Posch, M., Rafaj, P., Sandler, R., Schöpp, W., Wagner, F., and Winiwarter, W.: Cost-effective control of air quality and greenhouse gases in Europe: modeling and policy applications, Environ. Modell. Softw., 26, 1489–1501, <ext-link xlink:href="https://doi.org/10.1016/j.envsoft.2011.07.012" ext-link-type="DOI">10.1016/j.envsoft.2011.07.012</ext-link>, 2011.</mixed-citation></ref>
      <ref id="bib1.bib2"><label>2</label><mixed-citation>Bey, I., Jacob, D. J., Yantosca, R. M., Logan, J. A., Field, B. D., Fiore, A. M., Li, Q., Liu, H. Y., Mickley, L. J., and Schultz, M. G.: Global modeling of tropospheric chemistry with assimilated meteorology: model description and evaluation, J. Geophys. Res., 106, 23073–23095, <ext-link xlink:href="https://doi.org/10.1029/2001JD000807" ext-link-type="DOI">10.1029/2001JD000807</ext-link>, 2001.</mixed-citation></ref>
      <ref id="bib1.bib3"><label>3</label><mixed-citation>Boersma, K. F., Eskes, H. J., Veefkind, J. P., Brinksma, E. J., van der A, R. J., Sneep, M., van den Oord, G. H. J., Levelt, P. F., Stammes, P., Gleason, J. F., and Bucsela, E. J.: Near-real time retrieval of tropospheric <inline-formula><mml:math id="M372" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> from OMI, Atmos. Chem. Phys., 7, 2103–2118, <ext-link xlink:href="https://doi.org/10.5194/acp-7-2103-2007" ext-link-type="DOI">10.5194/acp-7-2103-2007</ext-link>, 2007.</mixed-citation></ref>
      <ref id="bib1.bib4"><label>4</label><mixed-citation>Boersma, K. F., Eskes, H. J., Dirksen, R. J., van der A, R. J., Veefkind, J. P., Stammes, P., Huijnen, V., Kleipool, Q. L., Sneep, M., Claas, J., Leitão, J., Richter, A., Zhou, Y., and Brunner, D.: An improved tropospheric <inline-formula><mml:math id="M373" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> column retrieval algorithm for the Ozone Monitoring Instrument, Atmos. Meas. Tech., 4, 1905–1928, <ext-link xlink:href="https://doi.org/10.5194/amt-4-1905-2011" ext-link-type="DOI">10.5194/amt-4-1905-2011</ext-link>, 2011.</mixed-citation></ref>
      <ref id="bib1.bib5"><label>5</label><mixed-citation>Chen, D., Wang, Y., McElroy, M. B., He, K., Yantosca, R. M., and Le Sager, P.: Regional CO pollution and export in China simulated by the high-resolution nested-grid GEOS-Chem model, Atmos. Chem. Phys., 9, 3825–3839, <ext-link xlink:href="https://doi.org/10.5194/acp-9-3825-2009" ext-link-type="DOI">10.5194/acp-9-3825-2009</ext-link>, 2009.</mixed-citation></ref>
      <ref id="bib1.bib6"><label>6</label><mixed-citation>Cooper, M., Martin, R. V., Padmanabhan, A., and Henze, D. K.: Comparing mass balance and adjoint methods for inverse modeling of nitrogen dioxide columns for global nitrogen oxide emissions, J. Geophys. Res., 122, 4718–4734, <ext-link xlink:href="https://doi.org/10.1002/2016JD025985" ext-link-type="DOI">10.1002/2016JD025985</ext-link>, 2017.</mixed-citation></ref>
      <ref id="bib1.bib7"><label>7</label><mixed-citation>Ding, J., Miyazaki, K., van der A, R. J., Mijling, B., Kurokawa, J.-I., Cho, S., Janssens-Maenhout, G., Zhang, Q., Liu, F., and Levelt, P. F.: Intercomparison of <inline-formula><mml:math id="M374" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> emission inventories over East Asia, Atmos. Chem. Phys., 17, 10125–10141, <ext-link xlink:href="https://doi.org/10.5194/acp-17-10125-2017" ext-link-type="DOI">10.5194/acp-17-10125-2017</ext-link>, 2017.</mixed-citation></ref>
      <ref id="bib1.bib8"><label>8</label><mixed-citation>Duan, L., Yu, Q., Zhang, Q., Wang, Z., Pan, Y., Larssen, T., Tang, J., and Mulder, J.: Acid deposition in Asia: emissions, deposition, and ecosystem effects, Atmos. Environ., 146, 55–69, <ext-link xlink:href="https://doi.org/10.1016/j.atmosenv.2016.07.018" ext-link-type="DOI">10.1016/j.atmosenv.2016.07.018</ext-link>, 2016.</mixed-citation></ref>
      <ref id="bib1.bib9"><label>9</label><mixed-citation>Fu, X., Wang, S., Zhao, B., Xing, J., Cheng, Z., Liu, H., and Hao, J.: Emission inventory of primary pollutants and chemical speciation in 2010 for the Yangtze River Delta region, China, Atmos. Environ., 70, 39–50, <ext-link xlink:href="https://doi.org/10.1016/j.atmosenv.2012.12.034" ext-link-type="DOI">10.1016/j.atmosenv.2012.12.034</ext-link>, 2013.</mixed-citation></ref>
      <ref id="bib1.bib10"><label>10</label><mixed-citation>Galmarini, S., Koffi, B., Solazzo, E., Keating, T., Hogrefe, C., Schulz, M., Benedictow, A., Griesfeller, J. J., Janssens-Maenhout, G., Carmichael, G., Fu, J., and Dentener, F.: Technical note: Coordination and harmonization of the multi-scale, multi-model activities HTAP2, AQMEII3, and MICS-Asia3: simulations, emission inventories, boundary conditions, and model output formats, Atmos. Chem. Phys., 17, 1543–1555, <ext-link xlink:href="https://doi.org/10.5194/acp-17-1543-2017" ext-link-type="DOI">10.5194/acp-17-1543-2017</ext-link>, 2017.</mixed-citation></ref>
      <ref id="bib1.bib11"><label>11</label><mixed-citation>Geng, G., Zhang, Q., Martin, R. V., Lin, J., Huo, H., Zheng, B., Wang, S., and He, K.: Impact of spatial proxies on the representation of bottom-up emission inventories: A satellite-based analysis, Atmos. Chem. Phys., 17, 4131–4145, <ext-link xlink:href="https://doi.org/10.5194/acp-17-4131-2017" ext-link-type="DOI">10.5194/acp-17-4131-2017</ext-link>, 2017.</mixed-citation></ref>
      <ref id="bib1.bib12"><label>12</label><mixed-citation>Granier, C., Bessagnet, B., Bond, T., D'Angiola, A., van der Gon, H. D., Frost, G. J., Heil, A., Kaiser, J. W., Kinne, S., Klimont, Z., Kloster, S., Lamarque, J.-F., Liousse, C., Masui, T., Meleux, F., Mieville, A., Ohara, T., Raut, J.-C., Riahi, K., Schultz, M. G., Smith, S. J., Thompson, A., van Aardenne, J., van der Werf, G. R., and van Vuuren, D. P.: Evolution of anthropogenic and biomass burning emissions of air pollutants at global and regional scales during the 1980–2010 period, Climatic Change, 109, 163–190, <ext-link xlink:href="https://doi.org/10.1007/s10584-011-0154-1" ext-link-type="DOI">10.1007/s10584-011-0154-1</ext-link>, 2011.</mixed-citation></ref>
      <ref id="bib1.bib13"><label>13</label><mixed-citation>Gu, D., Wang, Y., Smeltzer, C., and Liu, Z.: Reduction in <inline-formula><mml:math id="M375" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> emission trends over China: regional and seasonal variations, Environ. Sci. Technol., 47, 12912–12919, 2013.</mixed-citation></ref>
      <ref id="bib1.bib14"><label>14</label><mixed-citation>Gu, D., Wang, Y., Yin, R., Zhang, Y., and Smeltzer, C.: Inverse modelling of <inline-formula><mml:math id="M376" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> emissions over eastern China: uncertainties due to chemical non-linearity, Atmos. Meas. Tech., 9, 5193–5201, <ext-link xlink:href="https://doi.org/10.5194/amt-9-5193-2016" ext-link-type="DOI">10.5194/amt-9-5193-2016</ext-link>, 2016.</mixed-citation></ref>
      <ref id="bib1.bib15"><label>15</label><mixed-citation>Guan, D., Liu, Z., Geng, Y., Lindner, S., and Hubacek, K.: The gigatonne gap in China's carbon dioxide inventories, Nat. Clim. Change, 2, 672–675, <ext-link xlink:href="https://doi.org/10.1038/nclimate1560" ext-link-type="DOI">10.1038/nclimate1560</ext-link>, 2012.</mixed-citation></ref>
      <ref id="bib1.bib16"><label>16</label><mixed-citation>Hoesly, R. M., Smith, S. J., Feng, L., Klimont, Z., Janssens-Maenhout, G., Pitkanen, T., Seibert, J. J., Vu, L., Andres, R. J., Bolt, R. M., Bond, T. C., Dawidowski, L., Kholod, N., Kurokawa, J.-I., Li, M., Liu, L., Lu, Z., Moura, M. C. P., O'Rourke, P. R., and Zhang, Q.: Historical (1750–2014) anthropogenic emissions of reactive gases and aerosols from the Community Emissions Data System (CEDS), Geosci. Model Dev., 11, 369–408, <ext-link xlink:href="https://doi.org/10.5194/gmd-11-369-2018" ext-link-type="DOI">10.5194/gmd-11-369-2018</ext-link>, 2018.</mixed-citation></ref>
      <ref id="bib1.bib17"><label>17</label><mixed-citation>Hong, C., Zhang, Q., He, K., Guan, D., Li, M., Liu, F., and Zheng, B.: Variations of China's emission estimates: response to uncertainties in energy statistics, Atmos. Chem. Phys., 17, 1227-1239, <ext-link xlink:href="https://doi.org/10.5194/acp-17-1227-2017" ext-link-type="DOI">10.5194/acp-17-1227-2017</ext-link>, 2017.</mixed-citation></ref>
      <ref id="bib1.bib18"><label>18</label><mixed-citation>Huang, X., Song, Y., Li, M., Li, J., Huo, Q., Cai, X., Zhu, T., Hu, M., and
Zhang, H.: A high-resolution ammonia emission inventory in China, Global
Biogeochem. Cy., 26, GB1030, <ext-link xlink:href="https://doi.org/10.1029/2011GB004161" ext-link-type="DOI">10.1029/2011GB004161</ext-link>, 2012.</mixed-citation></ref>
      <ref id="bib1.bib19"><label>19</label><mixed-citation>
International Energy Agency (IEA): World Energy Statistics and Balances (2012 edition), IEA, Paris, 2012.</mixed-citation></ref>
      <ref id="bib1.bib20"><label>20</label><mixed-citation>Klimont, Z., Cofala, J., Xing, J., Wei, W., Zhang, C., Wang, S., Kejun, J., Bhandari, P., Mathur, R., Purohit, P., Rafaj, P., Chambers, A., Amann, M., and Hao, J.: Projections of <inline-formula><mml:math id="M377" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>, <inline-formula><mml:math id="M378" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> and carbonaceous aerosols emissions in Asia, Tellus B, 61, 602–617, <ext-link xlink:href="https://doi.org/10.1111/j.1600-0889.2009.00428.x" ext-link-type="DOI">10.1111/j.1600-0889.2009.00428.x</ext-link>, 2009.</mixed-citation></ref>
      <ref id="bib1.bib21"><label>21</label><mixed-citation>Klimont, Z., Smith, S. J., and Cofala, J.: The last decade of global
anthropogenic sulfur dioxide: 2000–2011 emissions, Environ. Res. Lett., 8,
014003, <ext-link xlink:href="https://doi.org/10.1088/1748-9326/8/1/014003" ext-link-type="DOI">10.1088/1748-9326/8/1/014003</ext-link>, 2013.</mixed-citation></ref>
      <ref id="bib1.bib22"><label>22</label><mixed-citation>Klimont, Z., Kupiainen, K., Heyes, C., Purohit, P., Cofala, J., Rafaj, P., Borken-Kleefeld, J., and Schöpp, W.: Global anthropogenic emissions of particulate matter including black carbon, Atmos. Chem. Phys., 17, 8681–8723, <ext-link xlink:href="https://doi.org/10.5194/acp-17-8681-2017" ext-link-type="DOI">10.5194/acp-17-8681-2017</ext-link>, 2017.</mixed-citation></ref>
      <ref id="bib1.bib23"><label>23</label><mixed-citation>Krotkov, N. A., McLinden, C. A., Li, C., Lamsal, L. N., Celarier, E. A., Marchenko, S. V., Swartz, W. H., Bucsela, E. J., Joiner, J., Duncan, B. N., Boersma, K. F., Veefkind, J. P., Levelt, P. F., Fioletov, V. E., Dickerson, R. R., He, H., Lu, Z., and Streets, D. G.: Aura OMI observations of regional SO<inline-formula><mml:math id="M379" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> and NO<inline-formula><mml:math id="M380" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> pollution changes from 2005 to 2015, Atmos. Chem. Phys., 16, 4605–4629, <ext-link xlink:href="https://doi.org/10.5194/acp-16-4605-2016" ext-link-type="DOI">10.5194/acp-16-4605-2016</ext-link>, 2016.</mixed-citation></ref>
      <ref id="bib1.bib24"><label>24</label><mixed-citation>Kurokawa, J., Ohara, T., Morikawa, T., Hanayama, S., Janssens-Maenhout, G., Fukui, T., Kawashima, K., and Akimoto, H.: Emissions of air pollutants and greenhouse gases over Asian regions during 2000–2008: Regional Emission inventory in ASia (REAS) version 2, Atmos. Chem. Phys., 13, 11019–11058, <ext-link xlink:href="https://doi.org/10.5194/acp-13-11019-2013" ext-link-type="DOI">10.5194/acp-13-11019-2013</ext-link>, 2013.</mixed-citation></ref>
      <ref id="bib1.bib25"><label>25</label><mixed-citation>Lamarque, J.-F., Bond, T. C., Eyring, V., Granier, C., Heil, A., Klimont, Z., Lee, D., Liousse, C., Mieville, A., Owen, B., Schultz, M. G., Shindell, D., Smith, S. J., Stehfest, E., Van Aardenne, J., Cooper, O. R., Kainuma, M., Mahowald, N., McConnell, J. R., Naik, V., Riahi, K., and van Vuuren, D. P.: Historical (1850–2000) gridded anthropogenic and biomass burning emissions of reactive gases and aerosols: methodology and application, Atmos. Chem. Phys., 10, 7017–7039, <ext-link xlink:href="https://doi.org/10.5194/acp-10-7017-2010" ext-link-type="DOI">10.5194/acp-10-7017-2010</ext-link>, 2010.</mixed-citation></ref>
      <ref id="bib1.bib26"><label>26</label><mixed-citation>Lamsal, L. N., Martin, R. V., Padmanabhan, A., van Donkelaar, A., Zhang, Q.,
Sioris, C. E., Chance, K., Kurosu, T. P., and Newchurch, M. J.: Application
of satellite observations for timely updates to global anthropogenic
<inline-formula><mml:math id="M381" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> emission inventories, Geophys. Res. Lett., 38, L05810,
<ext-link xlink:href="https://doi.org/10.1029/2010GL046476" ext-link-type="DOI">10.1029/2010GL046476</ext-link>, 2011.</mixed-citation></ref>
      <ref id="bib1.bib27"><label>27</label><mixed-citation>Lee, C., Martin, R. V., van Donkelaar, A., Lee, H., Dickerson, R. R., Hains, J. C., Krotkov, N., Richter, A., Vinnikov, K., and Schwab, J. J.: <inline-formula><mml:math id="M382" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> emissions and lifetimes: estimates from inverse modeling using in situ and global, space-based (SCIAMACHY and OMI) observations, J. Geophys. Res., 116, D06304, <ext-link xlink:href="https://doi.org/10.1029/2010JD014758" ext-link-type="DOI">10.1029/2010JD014758</ext-link>, 2011.</mixed-citation></ref>
      <ref id="bib1.bib28"><label>28</label><mixed-citation>Lei, Y., Zhang, Q., He, K. B., and Streets, D. G.: Primary anthropogenic aerosol emission trends for China, 1990–2005, Atmos. Chem. Phys., 11, 931–954, <ext-link xlink:href="https://doi.org/10.5194/acp-11-931-2011" ext-link-type="DOI">10.5194/acp-11-931-2011</ext-link>, 2011.</mixed-citation></ref>
      <ref id="bib1.bib29"><label>29</label><mixed-citation>Levelt, P. F., van den Oord, G. H. J., Dobber, M. R., Malkki, A., Huib, V., de Vries, J., Stammes, P., Lundell, J. O. V., and Saari, H.: The ozone monitoring instrument, IEEE T. Geosci. Remote, 44, 1093–1101, <ext-link xlink:href="https://doi.org/10.1109/TGRS.2006.872333" ext-link-type="DOI">10.1109/TGRS.2006.872333</ext-link>, 2006.</mixed-citation></ref>
      <ref id="bib1.bib30"><label>30</label><mixed-citation>Li, C., Krotkov, N. A., and Joiner, J.: OMI/aura sulphur dioxide (<inline-formula><mml:math id="M383" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>) total column 1-orbit L2 Swath <inline-formula><mml:math id="M384" display="inline"><mml:mrow><mml:mn mathvariant="normal">13</mml:mn><mml:mo>×</mml:mo><mml:mn mathvariant="normal">24</mml:mn></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math id="M385" display="inline"><mml:mi mathvariant="normal">km</mml:mi></mml:math></inline-formula> V003, Greenbelt, MD, USA, Goddard Earth Sciences Data and Information Services Center (GES DISC), <ext-link xlink:href="https://doi.org/10.5067/Aura/OMI/DATA2022" ext-link-type="DOI">10.5067/Aura/OMI/DATA2022</ext-link>, last access: November 2017, 2006.</mixed-citation></ref>
      <ref id="bib1.bib31"><label>31</label><mixed-citation>Li, M., Zhang, Q., Streets, D. G., He, K. B., Cheng, Y. F., Emmons, L. K., Huo, H., Kang, S. C., Lu, Z., Shao, M., Su, H., Yu, X., and Zhang, Y.: Mapping Asian anthropogenic emissions of non-methane volatile organic compounds to multiple chemical mechanisms, Atmos. Chem. Phys., 14, 5617–5638, <ext-link xlink:href="https://doi.org/10.5194/acp-14-5617-2014" ext-link-type="DOI">10.5194/acp-14-5617-2014</ext-link>, 2014.</mixed-citation></ref>
      <ref id="bib1.bib32"><label>32</label><mixed-citation>Li, M., Zhang, Q., Kurokawa, J.-I., Woo, J.-H., He, K., Lu, Z., Ohara, T., Song, Y., Streets, D. G., Carmichael, G. R., Cheng, Y., Hong, C., Huo, H., Jiang, X., Kang, S., Liu, F., Su, H., and Zheng, B.: MIX: a mosaic Asian anthropogenic emission inventory under the international collaboration framework of the MICS-Asia and HTAP, Atmos. Chem. Phys., 17, 935–963, <ext-link xlink:href="https://doi.org/10.5194/acp-17-935-2017" ext-link-type="DOI">10.5194/acp-17-935-2017</ext-link>, 2017.</mixed-citation></ref>
      <ref id="bib1.bib33"><label>33</label><mixed-citation>Lin, J.-T.: Satellite constraint for emissions of nitrogen oxides from anthropogenic, lightning and soil sources over East China on a high-resolution grid, Atmos. Chem. Phys., 12, 2881–2898, <ext-link xlink:href="https://doi.org/10.5194/acp-12-2881-2012" ext-link-type="DOI">10.5194/acp-12-2881-2012</ext-link>, 2012.</mixed-citation></ref>
      <ref id="bib1.bib34"><label>34</label><mixed-citation>Lin, J.-T., McElroy, M. B., and Boersma, K. F.: Constraint of anthropogenic <inline-formula><mml:math id="M386" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> emissions in China from different sectors: a new methodology using multiple satellite retrievals, Atmos. Chem. Phys., 10, 63–78, <ext-link xlink:href="https://doi.org/10.5194/acp-10-63-2010" ext-link-type="DOI">10.5194/acp-10-63-2010</ext-link>, 2010.</mixed-citation></ref>
      <ref id="bib1.bib35"><label>35</label><mixed-citation>Lin, J.-T., Martin, R. V., Boersma, K. F., Sneep, M., Stammes, P., Spurr, R., Wang, P., Van Roozendael, M., Clémer, K., and Irie, H.: Retrieving tropospheric nitrogen dioxide from the Ozone Monitoring Instrument: effects of aerosols, surface reflectance anisotropy, and vertical profile of nitrogen dioxide, Atmos. Chem. Phys., 14, 1441–1461, <ext-link xlink:href="https://doi.org/10.5194/acp-14-1441-2014" ext-link-type="DOI">10.5194/acp-14-1441-2014</ext-link>, 2014.</mixed-citation></ref>
      <ref id="bib1.bib36"><label>36</label><mixed-citation>Liu, F., Zhang, Q., Tong, D., Zheng, B., Li, M., Huo, H., and He, K. B.: High-resolution inventory of technologies, activities, and emissions of coal-fired power plants in China from 1990 to 2010, Atmos. Chem. Phys., 15, 13299–13317, <ext-link xlink:href="https://doi.org/10.5194/acp-15-13299-2015" ext-link-type="DOI">10.5194/acp-15-13299-2015</ext-link>, 2015.</mixed-citation></ref>
      <ref id="bib1.bib37"><label>37</label><mixed-citation>Liu, F., Beirle, S., Zhang, Q., Dörner, S., He, K., and Wagner, T.: <inline-formula><mml:math id="M387" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> lifetimes and emissions of cities and power plants in polluted  background estimated by satellite observations, Atmos. Chem. Phys., 16, 5283–5298, <ext-link xlink:href="https://doi.org/10.5194/acp-16-5283-2016" ext-link-type="DOI">10.5194/acp-16-5283-2016</ext-link>, 2016.</mixed-citation></ref>
      <ref id="bib1.bib38"><label>38</label><mixed-citation>Lu, Z., Streets, D. G., Zhang, Q., Wang, S., Carmichael, G. R., Cheng, Y. F., Wei, C., Chin, M., Diehl, T., and Tan, Q.: Sulfur dioxide emissions in China and sulfur trends in East Asia since 2000, Atmos. Chem. Phys., 10, 6311–6331, <ext-link xlink:href="https://doi.org/10.5194/acp-10-6311-2010" ext-link-type="DOI">10.5194/acp-10-6311-2010</ext-link>, 2010.</mixed-citation></ref>
      <ref id="bib1.bib39"><label>39</label><mixed-citation>Lu, Z., Zhang, Q., and Streets, D. G.: Sulfur dioxide and primary carbonaceous aerosol emissions in China and India, 1996–2010, Atmos. Chem. Phys., 11, 9839–9864, <ext-link xlink:href="https://doi.org/10.5194/acp-11-9839-2011" ext-link-type="DOI">10.5194/acp-11-9839-2011</ext-link>, 2011.</mixed-citation></ref>
      <ref id="bib1.bib40"><label>40</label><mixed-citation>Martin, R. V., Jacob, D. J., Chance, K., Kurosu, T. P., Palmer, P. I., and
Evans, M. J.: Global inventory of nitrogen oxide emissions constrained by
space-based observations of <inline-formula><mml:math id="M388" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">NO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> columns, J. Geophys. Res., 108, 4537,
<ext-link xlink:href="https://doi.org/10.1029/2003JD003453" ext-link-type="DOI">10.1029/2003JD003453</ext-link>, 2003.</mixed-citation></ref>
      <ref id="bib1.bib41"><label>41</label><mixed-citation>Miyazaki, K., Eskes, H., Sudo, K., Boersma, K. F., Bowman, K., and Kanaya, Y.: Decadal changes in global surface <inline-formula><mml:math id="M389" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> emissions from multi-constituent satellite data assimilation, Atmos. Chem. Phys., 17, 807–837, <ext-link xlink:href="https://doi.org/10.5194/acp-17-807-2017" ext-link-type="DOI">10.5194/acp-17-807-2017</ext-link>, 2017.</mixed-citation></ref>
      <ref id="bib1.bib42"><label>42</label><mixed-citation>Ohara, T., Akimoto, H., Kurokawa, J., Horii, N., Yamaji, K., Yan, X., and Hayasaka, T.: An Asian emission inventory of anthropogenic emission sources for the period 1980–2020, Atmos. Chem. Phys., 7, 4419–4444, <ext-link xlink:href="https://doi.org/10.5194/acp-7-4419-2007" ext-link-type="DOI">10.5194/acp-7-4419-2007</ext-link>, 2007.</mixed-citation></ref>
      <ref id="bib1.bib43"><label>43</label><mixed-citation>Palmer, P. I., Jacob, D. J., Chance, K., Martin, R. V., Spurr, R. J. D., Kurosu, T. P., Bey, I., Yantosca, R., Fiore, A., and Li, Q.: Air mass factor formulation for spectroscopic measurements from satellites: application to formaldehyde retrievals from the Global Ozone Monitoring Experiment, J. Geophys. Res., 106, 14539–14550, <ext-link xlink:href="https://doi.org/10.1029/2000jd900772" ext-link-type="DOI">10.1029/2000jd900772</ext-link>, 2001.</mixed-citation></ref>
      <ref id="bib1.bib44"><label>44</label><mixed-citation>Park, R. J., Jacob, D. J., Field, B. D., Yantosca, R. M., and Chin, M.:
Natural and transboundary pollution influences on sulfate-nitrate-ammonium
aerosols in the United States: implications for policy, J. Geophys. Res.,
109, D15204, <ext-link xlink:href="https://doi.org/10.1029/2003JD004473" ext-link-type="DOI">10.1029/2003JD004473</ext-link>, 2004.</mixed-citation></ref>
      <ref id="bib1.bib45"><label>45</label><mixed-citation>Rao, S., Klimont, Z., Smith, S. J., Van Dingenen, R., Dentener, F., Bouwman, L., Riahi, K., Amann, M., Bodirsky, B. L., van Vuuren, D. P., Aleluia Reis, L., Calvin, K., Drouet, L., Fricko, O., Fujimori, S., Gernaat, D., Havlik, P., Harmsen, M., Hasegawa, T., Heyes, C., Hilaire, J., Luderer, G., Masui, T., Stehfest, E., Strefler, J., van der Sluis, S., and Tavoni, M.: Future air pollution in the Shared Socio-economic Pathways, Global Environ. Chang., 42, 346–358, <ext-link xlink:href="https://doi.org/10.1016/j.gloenvcha.2016.05.012" ext-link-type="DOI">10.1016/j.gloenvcha.2016.05.012</ext-link>, 2017.</mixed-citation></ref>
      <ref id="bib1.bib46"><label>46</label><mixed-citation>
Riahi, K., Dentener, F., Gielen, D., Grubler, A., Jewell, J., Klimont, Z., Krey, V., McCollum, D., Pachauri, S., Rao, S., van Ruijven, B., van Vuuren, D. P., and Wilson, C.:  Energy pathways for sustainable development, Chapter 17, in: Global Energy Assessment – Toward a Sustainable Future, Cambridge University Press, Cambridge, UK and New York, NY, USA and the International Institute for Applied Systems Analysis, Laxenburg, Austria, 1203–1306, 2012.</mixed-citation></ref>
      <ref id="bib1.bib47"><label>47</label><mixed-citation>Saikawa, E., Kim, H., Zhong, M., Avramov, A., Zhao, Y., Janssens-Maenhout, G., Kurokawa, J.-I., Klimont, Z., Wagner, F., Naik, V., Horowitz, L. W., and Zhang, Q.: Comparison of emissions inventories of anthropogenic air pollutants and greenhouse gases in China, Atmos. Chem. Phys., 17, 6393–6421, <ext-link xlink:href="https://doi.org/10.5194/acp-17-6393-2017" ext-link-type="DOI">10.5194/acp-17-6393-2017</ext-link>, 2017.</mixed-citation></ref>
      <ref id="bib1.bib48"><label>48</label><mixed-citation>
Seinfeld, J. H. and Pandis, S. N.: Atmosppheric chemistry and physics: from air pollution to climate change, John Wiley &amp; Sons, New York, USA, 2006.</mixed-citation></ref>
      <ref id="bib1.bib49"><label>49</label><mixed-citation>Stohl, A., Aamaas, B., Amann, M., Baker, L. H., Bellouin, N., Berntsen, T. K., Boucher, O., Cherian, R., Collins, W., Daskalakis, N., Dusinska, M., Eckhardt, S., Fuglestvedt, J. S., Harju, M., Heyes, C., Hodnebrog, Ø., Hao, J., Im, U., Kanakidou, M., Klimont, Z., Kupiainen, K., Law, K. S., Lund, M. T., Maas, R., MacIntosh, C. R., Myhre, G., Myriokefalitakis, S., Olivié, D., Quaas, J., Quennehen, B., Raut, J.-C., Rumbold, S. T., Samset, B. H., Schulz, M., Seland, Ø., Shine, K. P., Skeie, R. B., Wang, S., Yttri, K. E., and Zhu, T.: Evaluating the climate and air quality impacts of  short-lived pollutants, Atmos. Chem. Phys., 15, 10529–10566, <ext-link xlink:href="https://doi.org/10.5194/acp-15-10529-2015" ext-link-type="DOI">10.5194/acp-15-10529-2015</ext-link>, 2015.</mixed-citation></ref>
      <ref id="bib1.bib50"><label>50</label><mixed-citation>Streets, D. G., Bond, T. C., Carmichael, G. R., Fernandes, S. D., Fu, Q.,
He, D., Klimont, Z., Nelson, S. M., Tsai, N. Y., Wang, M. Q., Woo, J. H., and
Yarber, K. F.: An inventory of gaseous and primary aerosol emissions in Asia
in the year 2000, J. Geophys. Res., 108, 8809, <ext-link xlink:href="https://doi.org/10.1029/2002JD003093" ext-link-type="DOI">10.1029/2002JD003093</ext-link>,
2003.</mixed-citation></ref>
      <ref id="bib1.bib51"><label>51</label><mixed-citation>Wang, S. W., Zhang, Q., Streets, D. G., He, K. B., Martin, R. V., Lamsal, L. N., Chen, D., Lei, Y., and Lu, Z.: Growth in <inline-formula><mml:math id="M390" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> emissions from power plants in China: bottom-up estimates and satellite observations, Atmos. Chem. Phys., 12, 4429–4447, <ext-link xlink:href="https://doi.org/10.5194/acp-12-4429-2012" ext-link-type="DOI">10.5194/acp-12-4429-2012</ext-link>, 2012.
</mixed-citation></ref><?xmltex \hack{\newpage}?>
      <ref id="bib1.bib52"><label>52</label><mixed-citation>Wang, S. X., Zhao, B., Cai, S. Y., Klimont, Z., Nielsen, C. P., Morikawa, T., Woo, J. H., Kim, Y., Fu, X., Xu, J. Y., Hao, J. M., and He, K. B.: Emission trends and mitigation options for air pollutants in East Asia, Atmos. Chem. Phys., 14, 6571–6603, <ext-link xlink:href="https://doi.org/10.5194/acp-14-6571-2014" ext-link-type="DOI">10.5194/acp-14-6571-2014</ext-link>, 2014.</mixed-citation></ref>
      <ref id="bib1.bib53"><label>53</label><mixed-citation>Zhang, Q., Streets, D. G., He, K., Wang, Y., Richter, A., Burrows, J. P., Uno, I., Jang, C. J., Chen, D., Yao, Z., and Lei, Y.: <inline-formula><mml:math id="M391" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> emission trends for China, 1995–2004: the view from the ground and the view from space, J. Geophys. Res., 112, D22306, <ext-link xlink:href="https://doi.org/10.1029/2007jd008684" ext-link-type="DOI">10.1029/2007jd008684</ext-link>, 2007.</mixed-citation></ref>
      <ref id="bib1.bib54"><label>54</label><mixed-citation>Zhang, Q., Streets, D. G., Carmichael, G. R., He, K. B., Huo, H., Kannari,
A., Klimont, Z., Park, I. S., Reddy, S., Fu, J. S., Chen, D., Duan, L., Lei,
Y., Wang, L. T., and Yao, Z. L.: Asian emissions in 2006 for the NASA INTEX-B
mission, Atmos. Chem. Phys., 9, 5131–5153, <ext-link xlink:href="https://doi.org/10.5194/acp-9-5131-2009" ext-link-type="DOI">10.5194/acp-9-5131-2009</ext-link>,
2009.</mixed-citation></ref>
      <ref id="bib1.bib55"><label>55</label><mixed-citation>Zhao, Y., Nielsen, C. P., Lei, Y., McElroy, M. B., and Hao, J.: Quantifying the uncertainties of a bottom-up emission inventory of anthropogenic atmospheric pollutants in China, Atmos. Chem. Phys., 11, 2295–2308, <ext-link xlink:href="https://doi.org/10.5194/acp-11-2295-2011" ext-link-type="DOI">10.5194/acp-11-2295-2011</ext-link>, 2011.</mixed-citation></ref>
      <ref id="bib1.bib56"><label>56</label><mixed-citation>Zhao, B., Wang, S. X., Liu, H., Xu, J. Y., Fu, K., Klimont, Z., Hao, J. M., He, K. B., Cofala, J., and Amann, M.: <inline-formula><mml:math id="M392" display="inline"><mml:mrow><mml:msub><mml:mtext>NO</mml:mtext><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> emissions in China: historical trends and future perspectives, Atmos. Chem. Phys., 13, 9869–9897, <ext-link xlink:href="https://doi.org/10.5194/acp-13-9869-2013" ext-link-type="DOI">10.5194/acp-13-9869-2013</ext-link>, 2013.</mixed-citation></ref>
      <ref id="bib1.bib57"><label>57</label><mixed-citation>Zhao, Y., Qiu, L. P., Xu, R. Y., Xie, F. J., Zhang, Q., Yu, Y. Y., Nielsen, C. P., Qin, H. X., Wang, H. K., Wu, X. C., Li, W. Q., and Zhang, J.: Advantages of a city-scale emission inventory for urban air quality research and policy: the case of Nanjing, a typical industrial city in the Yangtze River Delta, China, Atmos. Chem. Phys., 15, 12623–12644, <ext-link xlink:href="https://doi.org/10.5194/acp-15-12623-2015" ext-link-type="DOI">10.5194/acp-15-12623-2015</ext-link>, 2015.</mixed-citation></ref>
      <ref id="bib1.bib58"><label>58</label><mixed-citation>Zheng, B., Huo, H., Zhang, Q., Yao, Z. L., Wang, X. T., Yang, X. F., Liu, H., and He, K. B.: High-resolution mapping of vehicle emissions in China in 2008, Atmos. Chem. Phys., 14, 9787–9805, <ext-link xlink:href="https://doi.org/10.5194/acp-14-9787-2014" ext-link-type="DOI">10.5194/acp-14-9787-2014</ext-link>, 2014.</mixed-citation></ref>
      <ref id="bib1.bib59"><label>59</label><mixed-citation>Zheng, B., Zhang, Q., Tong, D., Chen, C., Hong, C., Li, M., Geng, G., Lei, Y., Huo, H., and He, K.: Resolution dependence of uncertainties in gridded emission inventories: a case study in Hebei, China, Atmos. Chem. Phys., 17, 921–933, <ext-link xlink:href="https://doi.org/10.5194/acp-17-921-2017" ext-link-type="DOI">10.5194/acp-17-921-2017</ext-link>, 2017.</mixed-citation></ref>
      <ref id="bib1.bib60"><label>60</label><mixed-citation>Zhou, Y., Zhao, Y., Mao, P., Zhang, Q., Zhang, J., Qiu, L., and Yang, Y.: Development of a high-resolution emission inventory and its evaluation and application through air quality modeling for Jiangsu Province, China, Atmos. Chem. Phys., 17, 211–233, <ext-link xlink:href="https://doi.org/10.5194/acp-17-211-2017" ext-link-type="DOI">10.5194/acp-17-211-2017</ext-link>, 2017.</mixed-citation></ref>

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    <!--<article-title-html>Comparison and evaluation of anthropogenic emissions of SO<sub>2</sub> and NO<sub><i>x</i></sub> over China</article-title-html>
<abstract-html><p class="p">Bottom-up emission inventories provide primary understanding of
sources of air pollution and essential input of chemical transport
models. Focusing on SO<sub>2</sub> and NO<sub><i>x</i></sub>, we conducted
a comprehensive evaluation of two widely used anthropogenic emission
inventories over China, ECLIPSE and MIX, to explore the potential
sources of uncertainties and find clues to improve emission
inventories. We first compared the activity rates and emission
factors used in two inventories and investigated the reasons of
differences and the impacts on emission estimates. We found that
SO<sub>2</sub> emission estimates are consistent between two
inventories (with 1 % differences), while NO<sub><i>x</i></sub>
emissions in ECLIPSE's estimates are 16 % lower than those of
MIX. The FGD (flue-gas desulfurization) device penetration rate and
removal efficiency, LNB (low-NO<sub><i>x</i></sub> burner) application
rate and abatement efficiency in power plants, emission factors of
industrial boilers and various vehicle types, and vehicle fleet need
further verification. Diesel consumptions are quite uncertain in
current inventories. Discrepancies at the sectorial and provincial levels
are much higher than those of the national total. We then examined
the impacts of different inventories on model performance by using
the nested GEOS-Chem model. We finally derived top-down emissions by
using the retrieved columns from the Ozone Monitoring Instrument
(OMI) compared with the bottom-up estimates. High correlations
were observed for SO<sub>2</sub> between model results and OMI
columns. For NO<sub><i>x</i></sub>, negative biases in bottom-up gridded
emission inventories (−21 % for MIX, −39 % for ECLIPSE)
were found compared to the satellite-based emissions. The emission trends
from 2005 to 2010 estimated by two inventories were both consistent
with satellite observations. The inventories appear to be fit for evaluation of
the policies at an aggregated or national level; more work is needed
in specific areas in order to improve the accuracy and robustness of
outcomes at finer spatial and also technological levels. To our
knowledge, this is the first work in which source comparisons
detailed to technology-level parameters are made along with the
remote sensing retrievals and chemical transport modeling.  Through
the comparison between bottom-up emission inventories and evaluation
with top-down information, we identified potential directions for
further improvement in inventory development.</p></abstract-html>
<ref-html id="bib1.bib1"><label>1</label><mixed-citation>
Amann, M., Bertok, I., Borken-Kleefeld, J., Cofala, J., Heyes, C., Höglund-Isaksson, L., Klimont, Z., Nguyen, B., Posch, M., Rafaj, P., Sandler, R., Schöpp, W., Wagner, F., and Winiwarter, W.: Cost-effective control of air quality and greenhouse gases in Europe: modeling and policy applications, Environ. Modell. Softw., 26, 1489–1501, <a href="https://doi.org/10.1016/j.envsoft.2011.07.012" target="_blank">https://doi.org/10.1016/j.envsoft.2011.07.012</a>, 2011.
</mixed-citation></ref-html>
<ref-html id="bib1.bib2"><label>2</label><mixed-citation>
Bey, I., Jacob, D. J., Yantosca, R. M., Logan, J. A., Field, B. D., Fiore, A. M., Li, Q., Liu, H. Y., Mickley, L. J., and Schultz, M. G.: Global modeling of tropospheric chemistry with assimilated meteorology: model description and evaluation, J. Geophys. Res., 106, 23073–23095, <a href="https://doi.org/10.1029/2001JD000807" target="_blank">https://doi.org/10.1029/2001JD000807</a>, 2001.
</mixed-citation></ref-html>
<ref-html id="bib1.bib3"><label>3</label><mixed-citation>
Boersma, K. F., Eskes, H. J., Veefkind, J. P., Brinksma, E. J., van der A, R. J., Sneep, M., van den Oord, G. H. J., Levelt, P. F., Stammes, P., Gleason, J. F., and Bucsela, E. J.: Near-real time retrieval of tropospheric NO<sub>2</sub> from OMI, Atmos. Chem. Phys., 7, 2103–2118, <a href="https://doi.org/10.5194/acp-7-2103-2007" target="_blank">https://doi.org/10.5194/acp-7-2103-2007</a>, 2007.
</mixed-citation></ref-html>
<ref-html id="bib1.bib4"><label>4</label><mixed-citation>
Boersma, K. F., Eskes, H. J., Dirksen, R. J., van der A, R. J., Veefkind, J. P., Stammes, P., Huijnen, V., Kleipool, Q. L., Sneep, M., Claas, J., Leitão, J., Richter, A., Zhou, Y., and Brunner, D.: An improved tropospheric NO<sub>2</sub> column retrieval algorithm for the Ozone Monitoring Instrument, Atmos. Meas. Tech., 4, 1905–1928, <a href="https://doi.org/10.5194/amt-4-1905-2011" target="_blank">https://doi.org/10.5194/amt-4-1905-2011</a>, 2011.
</mixed-citation></ref-html>
<ref-html id="bib1.bib5"><label>5</label><mixed-citation>
Chen, D., Wang, Y., McElroy, M. B., He, K., Yantosca, R. M., and Le Sager, P.: Regional CO pollution and export in China simulated by the high-resolution nested-grid GEOS-Chem model, Atmos. Chem. Phys., 9, 3825–3839, <a href="https://doi.org/10.5194/acp-9-3825-2009" target="_blank">https://doi.org/10.5194/acp-9-3825-2009</a>, 2009.
</mixed-citation></ref-html>
<ref-html id="bib1.bib6"><label>6</label><mixed-citation>
Cooper, M., Martin, R. V., Padmanabhan, A., and Henze, D. K.: Comparing mass balance and adjoint methods for inverse modeling of nitrogen dioxide columns for global nitrogen oxide emissions, J. Geophys. Res., 122, 4718–4734, <a href="https://doi.org/10.1002/2016JD025985" target="_blank">https://doi.org/10.1002/2016JD025985</a>, 2017.
</mixed-citation></ref-html>
<ref-html id="bib1.bib7"><label>7</label><mixed-citation>
Ding, J., Miyazaki, K., van der A, R. J., Mijling, B., Kurokawa, J.-I., Cho, S., Janssens-Maenhout, G., Zhang, Q., Liu, F., and Levelt, P. F.: Intercomparison of NO<sub><i>x</i></sub> emission inventories over East Asia, Atmos. Chem. Phys., 17, 10125–10141, <a href="https://doi.org/10.5194/acp-17-10125-2017" target="_blank">https://doi.org/10.5194/acp-17-10125-2017</a>, 2017.
</mixed-citation></ref-html>
<ref-html id="bib1.bib8"><label>8</label><mixed-citation>
Duan, L., Yu, Q., Zhang, Q., Wang, Z., Pan, Y., Larssen, T., Tang, J., and Mulder, J.: Acid deposition in Asia: emissions, deposition, and ecosystem effects, Atmos. Environ., 146, 55–69, <a href="https://doi.org/10.1016/j.atmosenv.2016.07.018" target="_blank">https://doi.org/10.1016/j.atmosenv.2016.07.018</a>, 2016.
</mixed-citation></ref-html>
<ref-html id="bib1.bib9"><label>9</label><mixed-citation> Fu, X., Wang, S., Zhao, B., Xing, J., Cheng, Z., Liu, H., and Hao, J.: Emission inventory of primary pollutants and chemical speciation in 2010 for the Yangtze River Delta region, China, Atmos. Environ., 70, 39–50, <a href="https://doi.org/10.1016/j.atmosenv.2012.12.034" target="_blank">https://doi.org/10.1016/j.atmosenv.2012.12.034</a>, 2013.
</mixed-citation></ref-html>
<ref-html id="bib1.bib10"><label>10</label><mixed-citation>
Galmarini, S., Koffi, B., Solazzo, E., Keating, T., Hogrefe, C., Schulz, M., Benedictow, A., Griesfeller, J. J., Janssens-Maenhout, G., Carmichael, G., Fu, J., and Dentener, F.: Technical note: Coordination and harmonization of the multi-scale, multi-model activities HTAP2, AQMEII3, and MICS-Asia3: simulations, emission inventories, boundary conditions, and model output formats, Atmos. Chem. Phys., 17, 1543–1555, <a href="https://doi.org/10.5194/acp-17-1543-2017" target="_blank">https://doi.org/10.5194/acp-17-1543-2017</a>, 2017.
</mixed-citation></ref-html>
<ref-html id="bib1.bib11"><label>11</label><mixed-citation>
Geng, G., Zhang, Q., Martin, R. V., Lin, J., Huo, H., Zheng, B., Wang, S., and He, K.: Impact of spatial proxies on the representation of bottom-up emission inventories: A satellite-based analysis, Atmos. Chem. Phys., 17, 4131–4145, <a href="https://doi.org/10.5194/acp-17-4131-2017" target="_blank">https://doi.org/10.5194/acp-17-4131-2017</a>, 2017.
</mixed-citation></ref-html>
<ref-html id="bib1.bib12"><label>12</label><mixed-citation>
Granier, C., Bessagnet, B., Bond, T., D'Angiola, A., van der Gon, H. D., Frost, G. J., Heil, A., Kaiser, J. W., Kinne, S., Klimont, Z., Kloster, S., Lamarque, J.-F., Liousse, C., Masui, T., Meleux, F., Mieville, A., Ohara, T., Raut, J.-C., Riahi, K., Schultz, M. G., Smith, S. J., Thompson, A., van Aardenne, J., van der Werf, G. R., and van Vuuren, D. P.: Evolution of anthropogenic and biomass burning emissions of air pollutants at global and regional scales during the 1980–2010 period, Climatic Change, 109, 163–190, <a href="https://doi.org/10.1007/s10584-011-0154-1" target="_blank">https://doi.org/10.1007/s10584-011-0154-1</a>, 2011.
</mixed-citation></ref-html>
<ref-html id="bib1.bib13"><label>13</label><mixed-citation>
Gu, D., Wang, Y., Smeltzer, C., and Liu, Z.: Reduction in NO<sub><i>x</i></sub> emission trends over China: regional and seasonal variations, Environ. Sci. Technol., 47, 12912–12919, 2013.
</mixed-citation></ref-html>
<ref-html id="bib1.bib14"><label>14</label><mixed-citation>
Gu, D., Wang, Y., Yin, R., Zhang, Y., and Smeltzer, C.: Inverse modelling of NO<sub><i>x</i></sub> emissions over eastern China: uncertainties due to chemical non-linearity, Atmos. Meas. Tech., 9, 5193–5201, <a href="https://doi.org/10.5194/amt-9-5193-2016" target="_blank">https://doi.org/10.5194/amt-9-5193-2016</a>, 2016.
</mixed-citation></ref-html>
<ref-html id="bib1.bib15"><label>15</label><mixed-citation>
Guan, D., Liu, Z., Geng, Y., Lindner, S., and Hubacek, K.: The gigatonne gap in China's carbon dioxide inventories, Nat. Clim. Change, 2, 672–675, <a href="https://doi.org/10.1038/nclimate1560" target="_blank">https://doi.org/10.1038/nclimate1560</a>, 2012.
</mixed-citation></ref-html>
<ref-html id="bib1.bib16"><label>16</label><mixed-citation>
Hoesly, R. M., Smith, S. J., Feng, L., Klimont, Z., Janssens-Maenhout, G., Pitkanen, T., Seibert, J. J., Vu, L., Andres, R. J., Bolt, R. M., Bond, T. C., Dawidowski, L., Kholod, N., Kurokawa, J.-I., Li, M., Liu, L., Lu, Z., Moura, M. C. P., O'Rourke, P. R., and Zhang, Q.: Historical (1750–2014) anthropogenic emissions of reactive gases and aerosols from the Community Emissions Data System (CEDS), Geosci. Model Dev., 11, 369–408, <a href="https://doi.org/10.5194/gmd-11-369-2018" target="_blank">https://doi.org/10.5194/gmd-11-369-2018</a>, 2018.
</mixed-citation></ref-html>
<ref-html id="bib1.bib17"><label>17</label><mixed-citation>
Hong, C., Zhang, Q., He, K., Guan, D., Li, M., Liu, F., and Zheng, B.: Variations of China's emission estimates: response to uncertainties in energy statistics, Atmos. Chem. Phys., 17, 1227-1239, <a href="https://doi.org/10.5194/acp-17-1227-2017" target="_blank">https://doi.org/10.5194/acp-17-1227-2017</a>, 2017.
</mixed-citation></ref-html>
<ref-html id="bib1.bib18"><label>18</label><mixed-citation>
Huang, X., Song, Y., Li, M., Li, J., Huo, Q., Cai, X., Zhu, T., Hu, M., and
Zhang, H.: A high-resolution ammonia emission inventory in China, Global
Biogeochem. Cy., 26, GB1030, <a href="https://doi.org/10.1029/2011GB004161" target="_blank">https://doi.org/10.1029/2011GB004161</a>, 2012.
</mixed-citation></ref-html>
<ref-html id="bib1.bib19"><label>19</label><mixed-citation>
International Energy Agency (IEA): World Energy Statistics and Balances (2012 edition), IEA, Paris, 2012.
</mixed-citation></ref-html>
<ref-html id="bib1.bib20"><label>20</label><mixed-citation>
Klimont, Z., Cofala, J., Xing, J., Wei, W., Zhang, C., Wang, S., Kejun, J., Bhandari, P., Mathur, R., Purohit, P., Rafaj, P., Chambers, A., Amann, M., and Hao, J.: Projections of SO<sub>2</sub>, NO<sub><i>x</i></sub> and carbonaceous aerosols emissions in Asia, Tellus B, 61, 602–617, <a href="https://doi.org/10.1111/j.1600-0889.2009.00428.x" target="_blank">https://doi.org/10.1111/j.1600-0889.2009.00428.x</a>, 2009.
</mixed-citation></ref-html>
<ref-html id="bib1.bib21"><label>21</label><mixed-citation>
Klimont, Z., Smith, S. J., and Cofala, J.: The last decade of global
anthropogenic sulfur dioxide: 2000–2011 emissions, Environ. Res. Lett., 8,
014003, <a href="https://doi.org/10.1088/1748-9326/8/1/014003" target="_blank">https://doi.org/10.1088/1748-9326/8/1/014003</a>, 2013.
</mixed-citation></ref-html>
<ref-html id="bib1.bib22"><label>22</label><mixed-citation>
Klimont, Z., Kupiainen, K., Heyes, C., Purohit, P., Cofala, J., Rafaj, P., Borken-Kleefeld, J., and Schöpp, W.: Global anthropogenic emissions of particulate matter including black carbon, Atmos. Chem. Phys., 17, 8681–8723, <a href="https://doi.org/10.5194/acp-17-8681-2017" target="_blank">https://doi.org/10.5194/acp-17-8681-2017</a>, 2017.
</mixed-citation></ref-html>
<ref-html id="bib1.bib23"><label>23</label><mixed-citation>
Krotkov, N. A., McLinden, C. A., Li, C., Lamsal, L. N., Celarier, E. A., Marchenko, S. V., Swartz, W. H., Bucsela, E. J., Joiner, J., Duncan, B. N., Boersma, K. F., Veefkind, J. P., Levelt, P. F., Fioletov, V. E., Dickerson, R. R., He, H., Lu, Z., and Streets, D. G.: Aura OMI observations of regional SO<sub>2</sub> and NO<sub>2</sub> pollution changes from 2005 to 2015, Atmos. Chem. Phys., 16, 4605–4629, <a href="https://doi.org/10.5194/acp-16-4605-2016" target="_blank">https://doi.org/10.5194/acp-16-4605-2016</a>, 2016.
</mixed-citation></ref-html>
<ref-html id="bib1.bib24"><label>24</label><mixed-citation>
Kurokawa, J., Ohara, T., Morikawa, T., Hanayama, S., Janssens-Maenhout, G., Fukui, T., Kawashima, K., and Akimoto, H.: Emissions of air pollutants and greenhouse gases over Asian regions during 2000–2008: Regional Emission inventory in ASia (REAS) version 2, Atmos. Chem. Phys., 13, 11019–11058, <a href="https://doi.org/10.5194/acp-13-11019-2013" target="_blank">https://doi.org/10.5194/acp-13-11019-2013</a>, 2013.
</mixed-citation></ref-html>
<ref-html id="bib1.bib25"><label>25</label><mixed-citation>
Lamarque, J.-F., Bond, T. C., Eyring, V., Granier, C., Heil, A., Klimont, Z., Lee, D., Liousse, C., Mieville, A., Owen, B., Schultz, M. G., Shindell, D., Smith, S. J., Stehfest, E., Van Aardenne, J., Cooper, O. R., Kainuma, M., Mahowald, N., McConnell, J. R., Naik, V., Riahi, K., and van Vuuren, D. P.: Historical (1850–2000) gridded anthropogenic and biomass burning emissions of reactive gases and aerosols: methodology and application, Atmos. Chem. Phys., 10, 7017–7039, <a href="https://doi.org/10.5194/acp-10-7017-2010" target="_blank">https://doi.org/10.5194/acp-10-7017-2010</a>, 2010.
</mixed-citation></ref-html>
<ref-html id="bib1.bib26"><label>26</label><mixed-citation>
Lamsal, L. N., Martin, R. V., Padmanabhan, A., van Donkelaar, A., Zhang, Q.,
Sioris, C. E., Chance, K., Kurosu, T. P., and Newchurch, M. J.: Application
of satellite observations for timely updates to global anthropogenic
NO<sub><i>x</i></sub> emission inventories, Geophys. Res. Lett., 38, L05810,
<a href="https://doi.org/10.1029/2010GL046476" target="_blank">https://doi.org/10.1029/2010GL046476</a>, 2011.
</mixed-citation></ref-html>
<ref-html id="bib1.bib27"><label>27</label><mixed-citation>
Lee, C., Martin, R. V., van Donkelaar, A., Lee, H., Dickerson, R. R., Hains, J. C., Krotkov, N., Richter, A., Vinnikov, K., and Schwab, J. J.: SO<sub>2</sub> emissions and lifetimes: estimates from inverse modeling using in situ and global, space-based (SCIAMACHY and OMI) observations, J. Geophys. Res., 116, D06304, <a href="https://doi.org/10.1029/2010JD014758" target="_blank">https://doi.org/10.1029/2010JD014758</a>, 2011.
</mixed-citation></ref-html>
<ref-html id="bib1.bib28"><label>28</label><mixed-citation>
Lei, Y., Zhang, Q., He, K. B., and Streets, D. G.: Primary anthropogenic aerosol emission trends for China, 1990–2005, Atmos. Chem. Phys., 11, 931–954, <a href="https://doi.org/10.5194/acp-11-931-2011" target="_blank">https://doi.org/10.5194/acp-11-931-2011</a>, 2011.
</mixed-citation></ref-html>
<ref-html id="bib1.bib29"><label>29</label><mixed-citation>
Levelt, P. F., van den Oord, G. H. J., Dobber, M. R., Malkki, A., Huib, V., de Vries, J., Stammes, P., Lundell, J. O. V., and Saari, H.: The ozone monitoring instrument, IEEE T. Geosci. Remote, 44, 1093–1101, <a href="https://doi.org/10.1109/TGRS.2006.872333" target="_blank">https://doi.org/10.1109/TGRS.2006.872333</a>, 2006.
</mixed-citation></ref-html>
<ref-html id="bib1.bib30"><label>30</label><mixed-citation>
Li, C., Krotkov, N. A., and Joiner, J.: OMI/aura sulphur dioxide (SO<sub>2</sub>) total column 1-orbit L2 Swath 13×24 km V003, Greenbelt, MD, USA, Goddard Earth Sciences Data and Information Services Center (GES DISC), <a href="https://doi.org/10.5067/Aura/OMI/DATA2022" target="_blank">https://doi.org/10.5067/Aura/OMI/DATA2022</a>, last access: November 2017, 2006.
</mixed-citation></ref-html>
<ref-html id="bib1.bib31"><label>31</label><mixed-citation>
Li, M., Zhang, Q., Streets, D. G., He, K. B., Cheng, Y. F., Emmons, L. K., Huo, H., Kang, S. C., Lu, Z., Shao, M., Su, H., Yu, X., and Zhang, Y.: Mapping Asian anthropogenic emissions of non-methane volatile organic compounds to multiple chemical mechanisms, Atmos. Chem. Phys., 14, 5617–5638, <a href="https://doi.org/10.5194/acp-14-5617-2014" target="_blank">https://doi.org/10.5194/acp-14-5617-2014</a>, 2014.
</mixed-citation></ref-html>
<ref-html id="bib1.bib32"><label>32</label><mixed-citation>
Li, M., Zhang, Q., Kurokawa, J.-I., Woo, J.-H., He, K., Lu, Z., Ohara, T., Song, Y., Streets, D. G., Carmichael, G. R., Cheng, Y., Hong, C., Huo, H., Jiang, X., Kang, S., Liu, F., Su, H., and Zheng, B.: MIX: a mosaic Asian anthropogenic emission inventory under the international collaboration framework of the MICS-Asia and HTAP, Atmos. Chem. Phys., 17, 935–963, <a href="https://doi.org/10.5194/acp-17-935-2017" target="_blank">https://doi.org/10.5194/acp-17-935-2017</a>, 2017.
</mixed-citation></ref-html>
<ref-html id="bib1.bib33"><label>33</label><mixed-citation>
Lin, J.-T.: Satellite constraint for emissions of nitrogen oxides from anthropogenic, lightning and soil sources over East China on a high-resolution grid, Atmos. Chem. Phys., 12, 2881–2898, <a href="https://doi.org/10.5194/acp-12-2881-2012" target="_blank">https://doi.org/10.5194/acp-12-2881-2012</a>, 2012.
</mixed-citation></ref-html>
<ref-html id="bib1.bib34"><label>34</label><mixed-citation>
Lin, J.-T., McElroy, M. B., and Boersma, K. F.: Constraint of anthropogenic NO<sub><i>x</i></sub> emissions in China from different sectors: a new methodology using multiple satellite retrievals, Atmos. Chem. Phys., 10, 63–78, <a href="https://doi.org/10.5194/acp-10-63-2010" target="_blank">https://doi.org/10.5194/acp-10-63-2010</a>, 2010.
</mixed-citation></ref-html>
<ref-html id="bib1.bib35"><label>35</label><mixed-citation>
Lin, J.-T., Martin, R. V., Boersma, K. F., Sneep, M., Stammes, P., Spurr, R., Wang, P., Van Roozendael, M., Clémer, K., and Irie, H.: Retrieving tropospheric nitrogen dioxide from the Ozone Monitoring Instrument: effects of aerosols, surface reflectance anisotropy, and vertical profile of nitrogen dioxide, Atmos. Chem. Phys., 14, 1441–1461, <a href="https://doi.org/10.5194/acp-14-1441-2014" target="_blank">https://doi.org/10.5194/acp-14-1441-2014</a>, 2014.
</mixed-citation></ref-html>
<ref-html id="bib1.bib36"><label>36</label><mixed-citation>
Liu, F., Zhang, Q., Tong, D., Zheng, B., Li, M., Huo, H., and He, K. B.: High-resolution inventory of technologies, activities, and emissions of coal-fired power plants in China from 1990 to 2010, Atmos. Chem. Phys., 15, 13299–13317, <a href="https://doi.org/10.5194/acp-15-13299-2015" target="_blank">https://doi.org/10.5194/acp-15-13299-2015</a>, 2015.
</mixed-citation></ref-html>
<ref-html id="bib1.bib37"><label>37</label><mixed-citation>
Liu, F., Beirle, S., Zhang, Q., Dörner, S., He, K., and Wagner, T.: NO<sub><i>x</i></sub> lifetimes and emissions of cities and power plants in polluted  background estimated by satellite observations, Atmos. Chem. Phys., 16, 5283–5298, <a href="https://doi.org/10.5194/acp-16-5283-2016" target="_blank">https://doi.org/10.5194/acp-16-5283-2016</a>, 2016.
</mixed-citation></ref-html>
<ref-html id="bib1.bib38"><label>38</label><mixed-citation>
Lu, Z., Streets, D. G., Zhang, Q., Wang, S., Carmichael, G. R., Cheng, Y. F., Wei, C., Chin, M., Diehl, T., and Tan, Q.: Sulfur dioxide emissions in China and sulfur trends in East Asia since 2000, Atmos. Chem. Phys., 10, 6311–6331, <a href="https://doi.org/10.5194/acp-10-6311-2010" target="_blank">https://doi.org/10.5194/acp-10-6311-2010</a>, 2010.
</mixed-citation></ref-html>
<ref-html id="bib1.bib39"><label>39</label><mixed-citation>
Lu, Z., Zhang, Q., and Streets, D. G.: Sulfur dioxide and primary carbonaceous aerosol emissions in China and India, 1996–2010, Atmos. Chem. Phys., 11, 9839–9864, <a href="https://doi.org/10.5194/acp-11-9839-2011" target="_blank">https://doi.org/10.5194/acp-11-9839-2011</a>, 2011.
</mixed-citation></ref-html>
<ref-html id="bib1.bib40"><label>40</label><mixed-citation>
Martin, R. V., Jacob, D. J., Chance, K., Kurosu, T. P., Palmer, P. I., and
Evans, M. J.: Global inventory of nitrogen oxide emissions constrained by
space-based observations of NO<sub>2</sub> columns, J. Geophys. Res., 108, 4537,
<a href="https://doi.org/10.1029/2003JD003453" target="_blank">https://doi.org/10.1029/2003JD003453</a>, 2003.
</mixed-citation></ref-html>
<ref-html id="bib1.bib41"><label>41</label><mixed-citation>
Miyazaki, K., Eskes, H., Sudo, K., Boersma, K. F., Bowman, K., and Kanaya, Y.: Decadal changes in global surface NO<sub><i>x</i></sub> emissions from multi-constituent satellite data assimilation, Atmos. Chem. Phys., 17, 807–837, <a href="https://doi.org/10.5194/acp-17-807-2017" target="_blank">https://doi.org/10.5194/acp-17-807-2017</a>, 2017.
</mixed-citation></ref-html>
<ref-html id="bib1.bib42"><label>42</label><mixed-citation>
Ohara, T., Akimoto, H., Kurokawa, J., Horii, N., Yamaji, K., Yan, X., and Hayasaka, T.: An Asian emission inventory of anthropogenic emission sources for the period 1980–2020, Atmos. Chem. Phys., 7, 4419–4444, <a href="https://doi.org/10.5194/acp-7-4419-2007" target="_blank">https://doi.org/10.5194/acp-7-4419-2007</a>, 2007.
</mixed-citation></ref-html>
<ref-html id="bib1.bib43"><label>43</label><mixed-citation>
Palmer, P. I., Jacob, D. J., Chance, K., Martin, R. V., Spurr, R. J. D., Kurosu, T. P., Bey, I., Yantosca, R., Fiore, A., and Li, Q.: Air mass factor formulation for spectroscopic measurements from satellites: application to formaldehyde retrievals from the Global Ozone Monitoring Experiment, J. Geophys. Res., 106, 14539–14550, <a href="https://doi.org/10.1029/2000jd900772" target="_blank">https://doi.org/10.1029/2000jd900772</a>, 2001.
</mixed-citation></ref-html>
<ref-html id="bib1.bib44"><label>44</label><mixed-citation>
Park, R. J., Jacob, D. J., Field, B. D., Yantosca, R. M., and Chin, M.:
Natural and transboundary pollution influences on sulfate-nitrate-ammonium
aerosols in the United States: implications for policy, J. Geophys. Res.,
109, D15204, <a href="https://doi.org/10.1029/2003JD004473" target="_blank">https://doi.org/10.1029/2003JD004473</a>, 2004.
</mixed-citation></ref-html>
<ref-html id="bib1.bib45"><label>45</label><mixed-citation>
Rao, S., Klimont, Z., Smith, S. J., Van Dingenen, R., Dentener, F., Bouwman, L., Riahi, K., Amann, M., Bodirsky, B. L., van Vuuren, D. P., Aleluia Reis, L., Calvin, K., Drouet, L., Fricko, O., Fujimori, S., Gernaat, D., Havlik, P., Harmsen, M., Hasegawa, T., Heyes, C., Hilaire, J., Luderer, G., Masui, T., Stehfest, E., Strefler, J., van der Sluis, S., and Tavoni, M.: Future air pollution in the Shared Socio-economic Pathways, Global Environ. Chang., 42, 346–358, <a href="https://doi.org/10.1016/j.gloenvcha.2016.05.012" target="_blank">https://doi.org/10.1016/j.gloenvcha.2016.05.012</a>, 2017.
</mixed-citation></ref-html>
<ref-html id="bib1.bib46"><label>46</label><mixed-citation>
Riahi, K., Dentener, F., Gielen, D., Grubler, A., Jewell, J., Klimont, Z., Krey, V., McCollum, D., Pachauri, S., Rao, S., van Ruijven, B., van Vuuren, D. P., and Wilson, C.:  Energy pathways for sustainable development, Chapter 17, in: Global Energy Assessment – Toward a Sustainable Future, Cambridge University Press, Cambridge, UK and New York, NY, USA and the International Institute for Applied Systems Analysis, Laxenburg, Austria, 1203–1306, 2012.
</mixed-citation></ref-html>
<ref-html id="bib1.bib47"><label>47</label><mixed-citation>
Saikawa, E., Kim, H., Zhong, M., Avramov, A., Zhao, Y., Janssens-Maenhout, G., Kurokawa, J.-I., Klimont, Z., Wagner, F., Naik, V., Horowitz, L. W., and Zhang, Q.: Comparison of emissions inventories of anthropogenic air pollutants and greenhouse gases in China, Atmos. Chem. Phys., 17, 6393–6421, <a href="https://doi.org/10.5194/acp-17-6393-2017" target="_blank">https://doi.org/10.5194/acp-17-6393-2017</a>, 2017.
</mixed-citation></ref-html>
<ref-html id="bib1.bib48"><label>48</label><mixed-citation>
Seinfeld, J. H. and Pandis, S. N.: Atmosppheric chemistry and physics: from air pollution to climate change, John Wiley &amp; Sons, New York, USA, 2006.
</mixed-citation></ref-html>
<ref-html id="bib1.bib49"><label>49</label><mixed-citation>
Stohl, A., Aamaas, B., Amann, M., Baker, L. H., Bellouin, N., Berntsen, T. K., Boucher, O., Cherian, R., Collins, W., Daskalakis, N., Dusinska, M., Eckhardt, S., Fuglestvedt, J. S., Harju, M., Heyes, C., Hodnebrog, Ø., Hao, J., Im, U., Kanakidou, M., Klimont, Z., Kupiainen, K., Law, K. S., Lund, M. T., Maas, R., MacIntosh, C. R., Myhre, G., Myriokefalitakis, S., Olivié, D., Quaas, J., Quennehen, B., Raut, J.-C., Rumbold, S. T., Samset, B. H., Schulz, M., Seland, Ø., Shine, K. P., Skeie, R. B., Wang, S., Yttri, K. E., and Zhu, T.: Evaluating the climate and air quality impacts of  short-lived pollutants, Atmos. Chem. Phys., 15, 10529–10566, <a href="https://doi.org/10.5194/acp-15-10529-2015" target="_blank">https://doi.org/10.5194/acp-15-10529-2015</a>, 2015.
</mixed-citation></ref-html>
<ref-html id="bib1.bib50"><label>50</label><mixed-citation>
Streets, D. G., Bond, T. C., Carmichael, G. R., Fernandes, S. D., Fu, Q.,
He, D., Klimont, Z., Nelson, S. M., Tsai, N. Y., Wang, M. Q., Woo, J. H., and
Yarber, K. F.: An inventory of gaseous and primary aerosol emissions in Asia
in the year 2000, J. Geophys. Res., 108, 8809, <a href="https://doi.org/10.1029/2002JD003093" target="_blank">https://doi.org/10.1029/2002JD003093</a>,
2003.
</mixed-citation></ref-html>
<ref-html id="bib1.bib51"><label>51</label><mixed-citation>
Wang, S. W., Zhang, Q., Streets, D. G., He, K. B., Martin, R. V., Lamsal, L. N., Chen, D., Lei, Y., and Lu, Z.: Growth in NO<sub><i>x</i></sub> emissions from power plants in China: bottom-up estimates and satellite observations, Atmos. Chem. Phys., 12, 4429–4447, <a href="https://doi.org/10.5194/acp-12-4429-2012" target="_blank">https://doi.org/10.5194/acp-12-4429-2012</a>, 2012.

</mixed-citation></ref-html>
<ref-html id="bib1.bib52"><label>52</label><mixed-citation>
Wang, S. X., Zhao, B., Cai, S. Y., Klimont, Z., Nielsen, C. P., Morikawa, T., Woo, J. H., Kim, Y., Fu, X., Xu, J. Y., Hao, J. M., and He, K. B.: Emission trends and mitigation options for air pollutants in East Asia, Atmos. Chem. Phys., 14, 6571–6603, <a href="https://doi.org/10.5194/acp-14-6571-2014" target="_blank">https://doi.org/10.5194/acp-14-6571-2014</a>, 2014.
</mixed-citation></ref-html>
<ref-html id="bib1.bib53"><label>53</label><mixed-citation>
Zhang, Q., Streets, D. G., He, K., Wang, Y., Richter, A., Burrows, J. P., Uno, I., Jang, C. J., Chen, D., Yao, Z., and Lei, Y.: NO<sub><i>x</i></sub> emission trends for China, 1995–2004: the view from the ground and the view from space, J. Geophys. Res., 112, D22306, <a href="https://doi.org/10.1029/2007jd008684" target="_blank">https://doi.org/10.1029/2007jd008684</a>, 2007.
</mixed-citation></ref-html>
<ref-html id="bib1.bib54"><label>54</label><mixed-citation>
Zhang, Q., Streets, D. G., Carmichael, G. R., He, K. B., Huo, H., Kannari,
A., Klimont, Z., Park, I. S., Reddy, S., Fu, J. S., Chen, D., Duan, L., Lei,
Y., Wang, L. T., and Yao, Z. L.: Asian emissions in 2006 for the NASA INTEX-B
mission, Atmos. Chem. Phys., 9, 5131–5153, <a href="https://doi.org/10.5194/acp-9-5131-2009" target="_blank">https://doi.org/10.5194/acp-9-5131-2009</a>,
2009.
</mixed-citation></ref-html>
<ref-html id="bib1.bib55"><label>55</label><mixed-citation>
Zhao, Y., Nielsen, C. P., Lei, Y., McElroy, M. B., and Hao, J.: Quantifying the uncertainties of a bottom-up emission inventory of anthropogenic atmospheric pollutants in China, Atmos. Chem. Phys., 11, 2295–2308, <a href="https://doi.org/10.5194/acp-11-2295-2011" target="_blank">https://doi.org/10.5194/acp-11-2295-2011</a>, 2011.
</mixed-citation></ref-html>
<ref-html id="bib1.bib56"><label>56</label><mixed-citation>
Zhao, B., Wang, S. X., Liu, H., Xu, J. Y., Fu, K., Klimont, Z., Hao, J. M., He, K. B., Cofala, J., and Amann, M.: NO<sub><i>x</i></sub> emissions in China: historical trends and future perspectives, Atmos. Chem. Phys., 13, 9869–9897, <a href="https://doi.org/10.5194/acp-13-9869-2013" target="_blank">https://doi.org/10.5194/acp-13-9869-2013</a>, 2013.
</mixed-citation></ref-html>
<ref-html id="bib1.bib57"><label>57</label><mixed-citation>
Zhao, Y., Qiu, L. P., Xu, R. Y., Xie, F. J., Zhang, Q., Yu, Y. Y., Nielsen, C. P., Qin, H. X., Wang, H. K., Wu, X. C., Li, W. Q., and Zhang, J.: Advantages of a city-scale emission inventory for urban air quality research and policy: the case of Nanjing, a typical industrial city in the Yangtze River Delta, China, Atmos. Chem. Phys., 15, 12623–12644, <a href="https://doi.org/10.5194/acp-15-12623-2015" target="_blank">https://doi.org/10.5194/acp-15-12623-2015</a>, 2015.
</mixed-citation></ref-html>
<ref-html id="bib1.bib58"><label>58</label><mixed-citation>
Zheng, B., Huo, H., Zhang, Q., Yao, Z. L., Wang, X. T., Yang, X. F., Liu, H., and He, K. B.: High-resolution mapping of vehicle emissions in China in 2008, Atmos. Chem. Phys., 14, 9787–9805, <a href="https://doi.org/10.5194/acp-14-9787-2014" target="_blank">https://doi.org/10.5194/acp-14-9787-2014</a>, 2014.
</mixed-citation></ref-html>
<ref-html id="bib1.bib59"><label>59</label><mixed-citation>
Zheng, B., Zhang, Q., Tong, D., Chen, C., Hong, C., Li, M., Geng, G., Lei, Y., Huo, H., and He, K.: Resolution dependence of uncertainties in gridded emission inventories: a case study in Hebei, China, Atmos. Chem. Phys., 17, 921–933, <a href="https://doi.org/10.5194/acp-17-921-2017" target="_blank">https://doi.org/10.5194/acp-17-921-2017</a>, 2017.
</mixed-citation></ref-html>
<ref-html id="bib1.bib60"><label>60</label><mixed-citation>
Zhou, Y., Zhao, Y., Mao, P., Zhang, Q., Zhang, J., Qiu, L., and Yang, Y.: Development of a high-resolution emission inventory and its evaluation and application through air quality modeling for Jiangsu Province, China, Atmos. Chem. Phys., 17, 211–233, <a href="https://doi.org/10.5194/acp-17-211-2017" target="_blank">https://doi.org/10.5194/acp-17-211-2017</a>, 2017.
</mixed-citation></ref-html>--></article>
