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<article xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:oasis="http://docs.oasis-open.org/ns/oasis-exchange/table" dtd-version="3.0"><?xmltex \makeatother\@nolinetrue\makeatletter?>
  <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-17-9261-2017</article-id><title-group><article-title>NO<inline-formula><mml:math id="M1" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emission trends over Chinese cities estimated from OMI observations during 2005 to 2015</article-title>
      </title-group><?xmltex \runningtitle{OMI-based NO${}_{{x}}$ emission trends over Chinese cities}?><?xmltex \runningauthor{F.~Liu et al.}?>
      <contrib-group>
        <contrib contrib-type="author" corresp="yes" rid="aff1 aff2 aff3 aff6 aff7">
          <name><surname>Liu</surname><given-names>Fei</given-names></name>
          <email>fei.liu@nasa.gov</email><email>liuf1010@gmail.com</email>
        <ext-link>https://orcid.org/0000-0002-0357-0274</ext-link></contrib>
        <contrib contrib-type="author" corresp="no" rid="aff3">
          <name><surname>Beirle</surname><given-names>Steffen</given-names></name>
          
        <ext-link>https://orcid.org/0000-0002-7196-0901</ext-link></contrib>
        <contrib contrib-type="author" corresp="yes" rid="aff1">
          <name><surname>Zhang</surname><given-names>Qiang</given-names></name>
          <email>qiangzhang@tsinghua.edu.cn</email>
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff2 aff5">
          <name><surname>van der A</surname><given-names>Ronald J.</given-names></name>
          
        <ext-link>https://orcid.org/0000-0002-0077-5338</ext-link></contrib>
        <contrib contrib-type="author" corresp="no" rid="aff4">
          <name><surname>Zheng</surname><given-names>Bo</given-names></name>
          
        <ext-link>https://orcid.org/0000-0001-8344-3445</ext-link></contrib>
        <contrib contrib-type="author" corresp="no" rid="aff1">
          <name><surname>Tong</surname><given-names>Dan</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff1 aff4">
          <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 of Earth System Science, <?xmltex \hack{\break}?> Tsinghua University, Beijing, China</institution>
        </aff>
        <aff id="aff2"><label>2</label><institution>Royal Netherlands Meteorological Institute (KNMI), P.O. Box 201, De
Bilt, the Netherlands</institution>
        </aff>
        <aff id="aff3"><label>3</label><institution>Max-Planck-Institut für Chemie, Mainz, Germany</institution>
        </aff>
        <aff id="aff4"><label>4</label><institution>State Key Joint Laboratory of Environment Simulation and Pollution
Control, School of Environment, Tsinghua University, Beijing, China</institution>
        </aff>
        <aff id="aff5"><label>5</label><institution>Nanjing University of Information Science &amp; Technology (NUIST),
Nanjing, China</institution>
        </aff>
        <aff id="aff6"><label>a</label><institution>now at: Universities Space Research Association (USRA), GESTAR,
Columbia, MD, USA</institution>
        </aff>
        <aff id="aff7"><label>b</label><institution>now at: NASA Goddard Space Flight Center, Greenbelt, MD, USA</institution>
        </aff>
      </contrib-group>
      <author-notes><corresp id="corr1">Fei Liu (fei.liu@nasa.gov, liuf1010@gmail.com) and Qiang Zhang (qiangzhang@tsinghua.edu.cn)</corresp></author-notes><pub-date><day>1</day><month>August</month><year>2017</year></pub-date>
      
      <volume>17</volume>
      <issue>15</issue>
      <fpage>9261</fpage><lpage>9275</lpage>
      <history>
        <date date-type="received"><day>23</day><month>April</month><year>2017</year></date>
           <date date-type="rev-request"><day>27</day><month>April</month><year>2017</year></date>
           <date date-type="rev-recd"><day>23</day><month>June</month><year>2017</year></date>
           <date date-type="accepted"><day>5</day><month>July</month><year>2017</year></date>
      </history>
      <permissions>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 3.0 Unported License. To view a copy of this licence, visit <ext-link ext-link-type="uri" xlink:href="https://creativecommons.org/licenses/by/3.0/">https://creativecommons.org/licenses/by/3.0/</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>Satellite nitrogen dioxide (NO<inline-formula><mml:math id="M2" display="inline"><mml:mrow><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:mo>)</mml:mo></mml:mrow></mml:math></inline-formula> observations have been widely used to
evaluate emission changes. To determine trends in nitrogen oxides (NO<inline-formula><mml:math id="M3" display="inline"><mml:mrow><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub><mml:mo>)</mml:mo></mml:mrow></mml:math></inline-formula>
emission over China, we used a method independent of chemical transport
models to quantify the NO<inline-formula><mml:math id="M4" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions from 48 cities and seven power
plants over China, on the basis of Ozone Monitoring Instrument (OMI) NO<inline-formula><mml:math id="M5" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula>
observations from 2005 to 2015. We found that NO<inline-formula><mml:math id="M6" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions over 48
Chinese cities increased by 52 % from 2005 to 2011 and decreased by
21 % from 2011 to 2015. The decrease since 2011 could be mainly
attributed to emission control measures in power sector; while cities with
different dominant emission sources (i.e., power, industrial, and
transportation sectors) showed variable emission decline timelines that
corresponded to the schedules for emission control in different sectors. The
time series of the derived NO<inline-formula><mml:math id="M7" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions was consistent with the
bottom-up emission inventories for all power plants (<inline-formula><mml:math id="M8" display="inline"><mml:mrow><mml:mi>r</mml:mi><mml:mo>=</mml:mo><mml:mn mathvariant="normal">0.8</mml:mn></mml:mrow></mml:math></inline-formula> on average), but
not for some cities (<inline-formula><mml:math id="M9" display="inline"><mml:mrow><mml:mi>r</mml:mi><mml:mo>=</mml:mo><mml:mn mathvariant="normal">0.4</mml:mn></mml:mrow></mml:math></inline-formula> on average). The lack of consistency observed
for cities was most probably due to the high uncertainty of bottom-up urban
emissions used in this study, which were derived from downscaling the
regional-based emission data to city level by using spatial distribution proxies.</p>
  </abstract>
    </article-meta>
  </front>
<body>
      

<sec id="Ch1.S1" sec-type="intro">
  <title>Introduction</title>
      <p>Nitrogen oxides (NO<inline-formula><mml:math id="M10" display="inline"><mml:mrow><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub><mml:mo>)</mml:mo></mml:mrow></mml:math></inline-formula>, including nitrogen dioxide (NO<inline-formula><mml:math id="M11" display="inline"><mml:mrow><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:mo>)</mml:mo></mml:mrow></mml:math></inline-formula> and nitric
oxide (NO), are atmospheric trace gases with a short lifetime, and they
actively participate in the formation of tropospheric ozone and secondary
aerosols and thus harm human health and significantly affect climate
(Seinfeld and Pandis, 2006). Anthropogenic activities, particularly fossil
fuel consumption, are the most important sources of NO<inline-formula><mml:math id="M12" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions.
Anthropogenic NO<inline-formula><mml:math id="M13" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions are clustered over densely populated urban
areas and suburban/rural industrial areas where large point sources such as
power plants are located.</p>
      <p>Tropospheric NO<inline-formula><mml:math id="M14" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> observations from space have been applied to infer the strength of NO<inline-formula><mml:math id="M15" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula>
emissions. The concentration of NO<inline-formula><mml:math id="M16" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> in a vertical column of air can be
measured via satellite instruments and related to NO<inline-formula><mml:math id="M17" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions
according to the mass balance by considering transport and chemical
conversion. A pioneering study has used the downwind decay of NO<inline-formula><mml:math id="M18" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> in
continental outflow regions to estimate the average NO<inline-formula><mml:math id="M19" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> lifetime and
global NO<inline-formula><mml:math id="M20" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions (Leue et al., 2001). Subsequent studies have used
chemical transport models (CTMs) to exploit satellite measurements as a
constraint to improve NO<inline-formula><mml:math id="M21" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emission inventories at the global/regional
scale (e.g., Martin et al., 2003; Konovalov et al., 2006; Kim et al., 2009;
Lamsal et al., 2011).</p>
      <p>The spatial and temporal resolution of tropospheric NO<inline-formula><mml:math id="M22" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> observed from
space has increased over time, from the Global Ozone Monitoring Experiment
(GOME), which was launched in 1995 (Burrows et al., 1999), to the Ozone
Monitoring Instrument (OMI) (Levelt et al., 2006), which was launched in 2004
and enables the use of satellite retrievals to resolve emissions at a finer
scale. OMI NO<inline-formula><mml:math id="M23" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> observations sorted according to wind direction from wind
fields developed by the European Center for Medium-range Weather Forecasting
(ECMWF) have been fitted by Beirle et al. (2011), who have used the
exponentially modified Gaussian function, which allows for a simultaneous fit
of the NO<inline-formula><mml:math id="M24" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> lifetime and emissions for megacities without further input
from CTMs. In the previous work, we advanced this method for estimating
NO<inline-formula><mml:math id="M25" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions from sources located in a polluted background (Liu et al.,
2016a). An alternative approach to quantifying urban NO<inline-formula><mml:math id="M26" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions,
proposed by Valin et al. (2013), involves rotating satellite observations
according to wind directions such that all observations are aligned in one
direction (from upwind to downwind), thus increasing the number of
observations. Subsequent studies have applied the concept of CTM-independent
methods for estimating SO<inline-formula><mml:math id="M27" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> by introducing an advanced three-dimensional
function (Fioletov et al., 2015, 2016; McLinden et al., 2016).</p>
      <p>Satellite observations are particularly suitable for evaluating emission
changes because they provide continuous and timely tropospheric NO<inline-formula><mml:math id="M28" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula>
measurements with global coverage (Lelieveld et al., 2015). Changes in the
spatial heterogeneity of NO<inline-formula><mml:math id="M29" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> trends have been observed worldwide, and
substantial decreases over Europe and the USA (Russell et al., 2012), as well
as
significant increases over Asia, have widely been detected in recent decades
(Richter et al., 2005). A linear function superposed on an annual seasonal
cycle has been introduced by van der A et al. (2008) to derive a
quantitative estimate of emission trends for a grid with a spatial
resolution of 1<inline-formula><mml:math id="M30" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> <inline-formula><mml:math id="M31" display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 1<inline-formula><mml:math id="M32" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> by fitting the
corresponding monthly NO<inline-formula><mml:math id="M33" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> columns. Follow-up studies (e.g., Schneider
and van der A, 2012; Schneider et al., 2015) have applied similar
statistical analyses to time series of NO<inline-formula><mml:math id="M34" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> in finer grid cells located
over the center of the city and have quantified the long-term average
pattern of NO<inline-formula><mml:math id="M35" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> for megacities. The multi-annual (moving) average is an
alternative method of describing local NO<inline-formula><mml:math id="M36" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> trends. The interannual
variation in the mass of a chemical species integrated around the source has
been used as an indicator of emission changes and has been shown to be
capable of illustrating the emission changes over US power plants (Fioletov
et al., 2011), Canadian oil sands (McLinden et al., 2012), and Indian power
plants (Lu et al., 2013). In addition, de Foy et al. (2015) and Lu et al.
(2015) have adopted the fitting function proposed by Beirle et al. (2011)
and have provided estimates of NO<inline-formula><mml:math id="M37" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emission trends from isolated power
plants and cities over the USA on the basis of 3-year average NO<inline-formula><mml:math id="M38" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> values
obtained through the plume rotation technique described by Valin et al.
(2013).</p>
      <p>China is one of the largest NO<inline-formula><mml:math id="M39" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emitters in the world and is the source
of approximately 18 % of the global NO<inline-formula><mml:math id="M40" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions (EDGAR 4.2,
EC-JRC/PBL, 2011). China has experienced rapid increases in NO<inline-formula><mml:math id="M41" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula>
emissions because of its growing economy over the past 2 decades, during
which emissions have increased by a factor of 3 (Kurokawa et al., 2013)
and have caused severe air pollution. To improve air quality, the Chinese
government implemented new emission regulations aimed at decreasing the
national total NO<inline-formula><mml:math id="M42" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions by 10 % between 2011 and 2015 (The State
Council of the People's Republic of China, 2011). Several recent studies
(e.g., Duncan et al., 2016; Krotkov et al., 2016) have suggested the
effectiveness of the air quality policy, as evidenced by a decreasing trend
in NO<inline-formula><mml:math id="M43" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> columns over China since 2012. Miyazaki et al. (2017), van der A
et al. (2017), and Souri et al. (2017) have further reported a recent decline
in national NO<inline-formula><mml:math id="M44" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions on the basis of satellite data assimilation.
Liu et al. (2016b) have studied changes in NO<inline-formula><mml:math id="M45" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> column densities for
each province from 2005 to 2015 and have performed an intercomparison of a
bottom-up inventory and satellite observations; the study attributes the
decline in regional NO<inline-formula><mml:math id="M46" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> to decreased emissions from power plants and
urban vehicles. However, few analyses have been performed for individual
cities or power plants, which are the primary targets of the new control
measures. Such investigations may provide stronger evidence of the effects
of control measures on NO<inline-formula><mml:math id="M47" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions.</p>
      <p>In this work, we quantified NO<inline-formula><mml:math id="M48" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emission trends over urban areas in
China from 2005 to 2015. Certain widely used approaches, including linear
trend analysis (e.g., Duncan et al., 2016; Krotkov et al., 2016) and
exponentially modified Gaussian method (e.g., de Foy et al., 2015; Lu et
al., 2015), are difficult to directly apply to hot spots in China. The
linear trend analysis approach is particularly useful for quantifying
changes for cities with a linear trend; however, it is not applicable to
most Chinese cities, which show a clear turning point of emissions. The
exponentially modified Gaussian method may introduce significant
uncertainties to the fit results because of the heterogeneously polluted
background over China (de Foy et al., 2014; Liu et al., 2016a). We applied
our advanced fitting function to sources located in a polluted background
(Liu et al., 2016a) to calculate the 3-year moving averages of NO<inline-formula><mml:math id="M49" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula>
emissions of pollution hotspots including individual cities and power
plants, and to relate their variations to bottom-up information. The main
purpose of this study was not only to demonstrate the recent decrease in
NO<inline-formula><mml:math id="M50" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> levels across the country, as indicated by previous reports (Liu et
al., 2016b), but also to display the diverse emission characteristics among
cities and provide in depth interpretations of these characteristics. The
fitting function and data sets used in this study are detailed in Sect. 2.
The interannual variations of NO<inline-formula><mml:math id="M51" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions and the analysis of
emission trends for cities derived from the fitting function are provided in
Sect. 3.1 and 3.2, respectively. The fitting results for cities are
presented in Sect. 3.3. The uncertainties associated with the fitting
results are discussed in Sect. 3.4, and the primary findings of this study
are summarized in Sect. 4.</p>
</sec>
<sec id="Ch1.S2">
  <title>Methodology</title>
<sec id="Ch1.S2.SS1">
  <title>Fitting method</title>
      <p>We improved the exponentially modified Gaussian method (Beirle et al., 2011)
to quantify the multi-year average NO<inline-formula><mml:math id="M52" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions obtained from OMI
NO<inline-formula><mml:math id="M53" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> observations for sources located in a polluted background (Liu et
al., 2016a). In this work, we adapted the fitting functions of Liu et al.
(2016a) to calculate the NO<inline-formula><mml:math id="M54" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions for individual cities and power
plants, including adjustments to meet the requirements of the trend
analysis.</p>
      <p>Consistently with our previous study (Liu et al., 2016a), we used the OMI
tropospheric NO<inline-formula><mml:math id="M55" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> (DOMINO) v2.0 product (Boersma et al., 2011) together
with the ECMWF ERA interim reanalysis (Dee et al., 2011) to perform the
analysis. We calculated the mean NO<inline-formula><mml:math id="M56" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> tropospheric vertical column
densities (TVCDs) for calm wind speeds below 2 m s<inline-formula><mml:math id="M57" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula> and eight
different wind direction sectors, by following the approach in Beirle et al.
(2011), and for weak-wind conditions (below 3 m s<inline-formula><mml:math id="M58" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula>), by following the
recommendations in Lu et al. (2015), from 2005 to 2015. We used only
non-winter data (from March to November) in order to avoid larger uncertainties because of
larger solar zenith angles and variable surface albedo (snow). In addition,
the longer NO<inline-formula><mml:math id="M59" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> lifetimes in winter resulted in a less direct
relationship between NO<inline-formula><mml:math id="M60" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions and satellite NO<inline-formula><mml:math id="M61" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> observations.</p>
      <p>Emissions were derived in a two-step approach in Liu et al. (2016a). The
first step was to use NO<inline-formula><mml:math id="M62" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> patterns under calm wind conditions as a
proxy for the spatial distribution of NO<inline-formula><mml:math id="M63" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions and determine the
effective atmospheric NO<inline-formula><mml:math id="M64" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> lifetime from the change of spatial patterns
measured at higher wind speeds. The second step was to derive emissions from
the NO<inline-formula><mml:math id="M65" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> mass integrated around the source of interest divided by the
corresponding lifetime.</p>
      <p>To perform a trend analysis, we adjusted the method as follows: we based the
estimation on NO<inline-formula><mml:math id="M66" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> columns around the source of interest averaged over
3 years, in agreement with previous studies (e.g., Fioletov et al.,
2011; Lu et al., 2015), and then the total NO<inline-formula><mml:math id="M67" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> mass was integrated over
the mean TVCDs at weak-wind speeds (below 3 m s<inline-formula><mml:math id="M68" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula>) instead of calm winds
(below 2 m s<inline-formula><mml:math id="M69" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula>) to balance the need for increasing the number of observations
and minimizing interferences by advection. Notably, we were not able to
derive valid lifetimes on the basis of the 3-year average NO<inline-formula><mml:math id="M70" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> columns;
instead, we fitted the lifetimes on the basis of multiple-year data (the
entire study period) because of the lack of sufficient observations for
different wind sectors within a 3-year period. Therefore, the NO<inline-formula><mml:math id="M71" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula>
emissions for each 3-year period were calculated by dividing the
corresponding total NO<inline-formula><mml:math id="M72" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> mass by the multiple-year average lifetime. In
this way, the temporal variations in NO<inline-formula><mml:math id="M73" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions were merely
dependent on the changes in the total NO<inline-formula><mml:math id="M74" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> mass, excluding background
pollution, assuming that the lifetimes did not change over time. However, we
wanted to include the fit over the lifetime in this study to make the
comparison of top-down and bottom-up estimates more straightforward.
Subsequently, we included mountainous sites, which were defined as sites
where the absolute difference in elevation between ECMWF and GTOPO data
(available at <uri>https://lta.cr.usgs.gov/GTOPO30</uri>; rescaled to 0.05<inline-formula><mml:math id="M75" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>)
was larger than 250 m, in the following analysis. Our previous findings
(Sect. 2.6 in Liu et al., 2016a) have indicated that appropriate wind fields,
which are required for accurate lifetime calculations, may not always be
achieved from the ECMWF simulation over mountainous regions. However,
depending on changes in the total NO<inline-formula><mml:math id="M76" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> mass, the fitted emission trends
are not as sensitive as the fitted lifetimes to wind fields; thus, we did
not exclude mountainous sites from the trend analysis. The fitting results
with poor performance (i.e., <inline-formula><mml:math id="M77" display="inline"><mml:mrow><mml:mi>R</mml:mi><mml:mi mathvariant="italic">&lt;</mml:mi><mml:mn mathvariant="normal">0.9</mml:mn></mml:mrow></mml:math></inline-formula>, lower bound of confidence
interval CI <inline-formula><mml:math id="M78" display="inline"><mml:mi mathvariant="italic">&lt;</mml:mi></mml:math></inline-formula> 0, CI width for lifetime <inline-formula><mml:math id="M79" display="inline"><mml:mi mathvariant="italic">&gt;</mml:mi></mml:math></inline-formula> 10 h, CI width
for the NO<inline-formula><mml:math id="M80" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> mass <inline-formula><mml:math id="M81" display="inline"><mml:mi mathvariant="italic">&gt;</mml:mi></mml:math></inline-formula> 0.8 <inline-formula><mml:math id="M82" display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> mass) were discarded, in
accordance with the criteria in Sect. 2.2 of Liu et al. (2016a).</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F1"><caption><p>Locations of the selected sites in this study. The triangles
represent the mountainous sites defined in Sect. 2.1. All locations are
labeled with their IDs (see Table S1).</p></caption>
          <?xmltex \igopts{width=241.848425pt}?><graphic xlink:href="https://acp.copernicus.org/articles/17/9261/2017/acp-17-9261-2017-f01.png"/>

        </fig>

      <p>We selected the Huolin power plant (site no. 2; 45.5<inline-formula><mml:math id="M83" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> N,
119.7<inline-formula><mml:math id="M84" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> E), which is located in Holingol, a county-level city of
Inner Mongolia, China (shown in Fig. 1), to demonstrate our approach. The
Huolin power plant has a total capacity of 2400 MW and dominates the
NO<inline-formula><mml:math id="M85" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions from the city of Holingol, contributing over 80 % of
the total emissions estimated by using the Multi-resolution Emission
Inventory for China (see Sect. 2.2), which is a bottom-up emission
inventory. Figure 2a displays the 3-year average NO<inline-formula><mml:math id="M86" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> TVCDs around the
power plant under weak-wind conditions from 2005 to 2015. For simplicity,
the 3-year period is represented by the middle year with an asterisk (e.g.,
2006<inline-formula><mml:math id="M87" display="inline"><mml:msup><mml:mi/><mml:mo>∗</mml:mo></mml:msup></mml:math></inline-formula> denotes the period from 2005 to 2007). A significant increase in TVCDs
was observed from 2006<inline-formula><mml:math id="M88" display="inline"><mml:msup><mml:mi/><mml:mo>∗</mml:mo></mml:msup></mml:math></inline-formula> to 2010<inline-formula><mml:math id="M89" display="inline"><mml:msup><mml:mi/><mml:mo>∗</mml:mo></mml:msup></mml:math></inline-formula>, which was followed by a
subsequent decrease. Figure 2b presents the fitted background and NO<inline-formula><mml:math id="M90" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula>
emissions. The fitted NO<inline-formula><mml:math id="M91" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions showed an increase of up to a
factor of 4 from 2006<inline-formula><mml:math id="M92" display="inline"><mml:msup><mml:mi/><mml:mo>∗</mml:mo></mml:msup></mml:math></inline-formula> to 2010<inline-formula><mml:math id="M93" display="inline"><mml:msup><mml:mi/><mml:mo>∗</mml:mo></mml:msup></mml:math></inline-formula> and a decrease of
30 % from 2011<inline-formula><mml:math id="M94" display="inline"><mml:msup><mml:mi/><mml:mo>∗</mml:mo></mml:msup></mml:math></inline-formula> to 2014<inline-formula><mml:math id="M95" display="inline"><mml:msup><mml:mi/><mml:mo>∗</mml:mo></mml:msup></mml:math></inline-formula>, whereas the fitted background
was steady and showed a standard deviation of less than 10 % from
2006<inline-formula><mml:math id="M96" display="inline"><mml:msup><mml:mi/><mml:mo>∗</mml:mo></mml:msup></mml:math></inline-formula> to 2014<inline-formula><mml:math id="M97" display="inline"><mml:msup><mml:mi/><mml:mo>∗</mml:mo></mml:msup></mml:math></inline-formula>. The growth of the fitted NO<inline-formula><mml:math id="M98" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula>
emissions in the early stage was found to be consistent with the
construction of new electric-generating units, with the total capacity
increasing from 300 to 2400 MW from 2005 to 2009. Subsequently, the
fitted NO<inline-formula><mml:math id="M99" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions remained steady from 2010<inline-formula><mml:math id="M100" display="inline"><mml:msup><mml:mi/><mml:mo>∗</mml:mo></mml:msup></mml:math></inline-formula> to 2012<inline-formula><mml:math id="M101" display="inline"><mml:msup><mml:mi/><mml:mo>∗</mml:mo></mml:msup></mml:math></inline-formula>, when no new electric-generating units were placed into service, and
finally decreased after the installation of selective catalytic reduction
(SCR) equipment at the power plants. This decrease in emissions indicated
the effectiveness of SCR equipment for decreasing emissions.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F2"><caption><p><bold>(a)</bold> OMI NO<inline-formula><mml:math id="M102" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> TVCD map under weak-wind conditions
(&lt; 3 m s<inline-formula><mml:math id="M103" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula>) around the Huolin power plant (no. 2 in Fig. 1)
during 2005 to 2015 and <bold>(b)</bold> the corresponding fit results. The red
and blue lines denote the fitted emissions and background, respectively; the
pink line denotes the bottom-up emission estimates; the solid and dashed bars
denote the total capacity of the generation units and the capacity of
generation units that installed SCR equipment, respectively. The information
on the capacity and SCR equipment is derived from the CPED database (Liu et
al., 2015). Error bars show the uncertainties for emissions by using this
method and bottom-up inventories (see Sect. 3.4).</p></caption>
          <?xmltex \igopts{width=236.157874pt}?><graphic xlink:href="https://acp.copernicus.org/articles/17/9261/2017/acp-17-9261-2017-f02.png"/>

        </fig>

</sec>
<sec id="Ch1.S2.SS2">
  <title>Bottom-up information</title>
      <p>We used bottom-up information to pre-select promising sites and to perform a
comparison with the fitted top-down emission trends. We selected bottom-up
emission inventories widely used in the community, in which multi-year
gridded estimates are provided (more than 3 years of data available from 2005
to 2015). We finally included Emission Database for Global Atmospheric
Research version 4.3 (EDGAR v4.3; available for 1970–2010; Crippa et al.
2016), Regional Emission inventory in Asia version 2.1 (REAS v2.1; available
for 2000–2008; Kurokawa et al., 2013), and the Multi-resolution Emission Inventory for China (MEIC;
<uri>http://www.meicmodel.org</uri>) compiled by Tsinghua University. The analysis
was focused on the MEIC inventory that are available for the whole period.
Vehicle population and coal consumption at the city level were derived from
the China Statistical Yearbook for Regional Economy (NBS: CSYRE, 2004–2014)
and the China Environment Yearbook (NBS: CEY, 2004–2015), respectively. We
derived the information for the coordinates, unit capacities, and
technologies for individual power plants from the unit-based China coal-fired
Power plant Emissions Database (CPED) (Liu et al., 2015) integrated in MEIC.</p>
      <p>We calculated the NO<inline-formula><mml:math id="M104" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions from cities and power plants from 2005
to 2015. Only emissions for non-winter seasons were considered, in accordance
with the emissions included for the top-down estimates, except for EDGAR in
which only annual emissions are available. The gridded bottom-up inventories
were integrated over a 40 km <inline-formula><mml:math id="M105" display="inline"><mml:mrow><mml:mo>×</mml:mo><mml:mn mathvariant="normal">40</mml:mn></mml:mrow></mml:math></inline-formula> km metropolitan area for which
the proposed top-down method was sensitive to calculate the total urban
emissions (Liu et al., 2016a). Emissions for individual power plants are
derived from CPED and the power plant sector of REAS directly (emissions from
individual point sources are not available in EDGAR). Notably, the emissions
uncertainties associated with power plants derived from CPED were much lower
(30 %) than those for cities (50–200 %) because the former was
calculated directly from unit-level information whereas the latter was
derived by downscaling regional-based emission data to finer grids using
spatial proxies and integrating emissions from corresponding grids.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F3" specific-use="star"><caption><p><bold>(a)</bold> Fitted (yellow bar) and total anthropogenic NO<inline-formula><mml:math id="M106" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula>
emissions by sector for all investigated cities in this study during 2005 to
2015. The emissions data are derived from the MEIC model.
<bold>(b)</bold> Interannual trends of the fitted (gray line) and bottom-up
anthropogenic NO<inline-formula><mml:math id="M107" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions for selected cities with valid information
on the vehicle population (blue solid squares) and coal consumption (blue
open squares) from 2005 to 2015. The emissions deriving from the MEIC, REAS
v2.1 and EDGAR v4.3 inventory are displayed in black, green, and purple,
respectively. The pink lines denote the ratio of the fitted NO<inline-formula><mml:math id="M108" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula>
emissions in this study to the vehicle population (solid squares) and coal
consumption (open squares). The relative changes of the vehicle population
and coal consumption are indicated by right axes. Error bars show the
uncertainties for the fitted emissions by using this method (see Sect. 3.4).</p></caption>
          <?xmltex \igopts{width=426.791339pt}?><graphic xlink:href="https://acp.copernicus.org/articles/17/9261/2017/acp-17-9261-2017-f03.png"/>

        </fig>

</sec>
<sec id="Ch1.S2.SS3">
  <title>Selection of locations</title>
      <p>We selected large cities and power plants in China as the pre-selected
sites for which bottom-up emission information was derived from the MEIC
and CPED inventories, respectively. China classifies its administrative
divisions into five practical levels (from large to small): province,
prefecture, county, township and village. Only prefecture-level cities were
selected for analysis in this study. Power plants with NO<inline-formula><mml:math id="M109" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emission
rates greater than 10 Gg yr<inline-formula><mml:math id="M110" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula> were selected for emission fitting. Figure 1
illustrates all investigated sites where the fit results showed good
performance. Among over 200 pre-selected cities, 48 cities (including 14
mountainous sites) were fitted with good performance (see the definition in
Sect. 2.1). While among over 100 pre-selected power plants, more than half
were excluded from the fit procedure because they are located in a radius
of 100 km around prefecture-level city centers, on the basis of a visual
inspection of satellite imagery from Google Earth. Only seven power plants
(including three mountainous sites) were fitted with good performance. Detailed
information on the sites is tabulated in Table S1 of the Supplement.</p>
</sec>
</sec>
<sec id="Ch1.S3">
  <title>Results and discussion</title>
<sec id="Ch1.S3.SS1">
  <?xmltex \opttitle{Interannual trends in OMI NO${}_{{x}}$ emissions for cities}?><title>Interannual trends in OMI NO<inline-formula><mml:math id="M111" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions for cities</title>
      <p>The trends in the fitted NO<inline-formula><mml:math id="M112" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions for 48 cities from 2006<inline-formula><mml:math id="M113" display="inline"><mml:msup><mml:mi/><mml:mo>∗</mml:mo></mml:msup></mml:math></inline-formula> to 2014<inline-formula><mml:math id="M114" display="inline"><mml:msup><mml:mi/><mml:mo>∗</mml:mo></mml:msup></mml:math></inline-formula> are shown in Fig. 3a, with an average growth trend of
52 % prior to 2011<inline-formula><mml:math id="M115" display="inline"><mml:msup><mml:mi/><mml:mo>∗</mml:mo></mml:msup></mml:math></inline-formula> for all investigated cities and a declining
trend of 21 % from 2011<inline-formula><mml:math id="M116" display="inline"><mml:msup><mml:mi/><mml:mo>∗</mml:mo></mml:msup></mml:math></inline-formula> to 2014<inline-formula><mml:math id="M117" display="inline"><mml:msup><mml:mi/><mml:mo>∗</mml:mo></mml:msup></mml:math></inline-formula>. The NO<inline-formula><mml:math id="M118" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula>
emissions over urban areas essentially represent a marker for
combustion-related emissions, including coal combustion for power generation
and industrial processes and oil combustion for transportation. Figure 3b
further summarizes the statistical data of industrial coal consumption (open
squares) and vehicle population (proxy of oil consumption, solid squares),
which are available for only 28 cities. Not surprisingly, the fitted
emission trends for the 28 cities (circles) were consistent with those for
the overall 48 cities. The observed sharp growth of 47 % in NO<inline-formula><mml:math id="M119" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula>
emissions during the period of 2006<inline-formula><mml:math id="M120" display="inline"><mml:msup><mml:mi/><mml:mo>∗</mml:mo></mml:msup></mml:math></inline-formula>–2011<inline-formula><mml:math id="M121" display="inline"><mml:msup><mml:mi/><mml:mo>∗</mml:mo></mml:msup></mml:math></inline-formula> was attributed
to the growth of 75 and 158 % in coal consumption and vehicle
population, respectively. Coal consumption and vehicle population continued
to rise and increased by 8 and 26 % from 2011<inline-formula><mml:math id="M122" display="inline"><mml:msup><mml:mi/><mml:mo>∗</mml:mo></mml:msup></mml:math></inline-formula> to 2014<inline-formula><mml:math id="M123" display="inline"><mml:msup><mml:mi/><mml:mo>∗</mml:mo></mml:msup></mml:math></inline-formula>, respectively; however, a subsequent decline in NO<inline-formula><mml:math id="M124" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions was
observed. We further divided these NO<inline-formula><mml:math id="M125" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions by coal consumption
and vehicle population because their respective temporal variations can be
treated as an approximation of the average emission factor trends in the
industrial (including power) and transportation sectors, on the basis of the
assumption that contributions of NO<inline-formula><mml:math id="M126" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions from corresponding
sectors are constant over time. The ratio of emissions to coal consumption
and vehicle population has diminished over time and decreased by 37 and
65 % from 2011<inline-formula><mml:math id="M127" display="inline"><mml:msup><mml:mi/><mml:mo>∗</mml:mo></mml:msup></mml:math></inline-formula> to 2014<inline-formula><mml:math id="M128" display="inline"><mml:msup><mml:mi/><mml:mo>∗</mml:mo></mml:msup></mml:math></inline-formula>, respectively. This declining
trend was greater than the fluctuations in contributions of NO<inline-formula><mml:math id="M129" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula>
emissions from the corresponding sectors (ranging from 1 to 24 % for
individual cities) and indicated the effectiveness of emission control
measures.</p>
      <p>The time series between fitted emissions and bottom-up inventories are
generally consistent in Fig. 3b. The changes in NO<inline-formula><mml:math id="M130" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions from 2005
to 2015 according to sector for the investigated cities on the basis of MEIC
estimates are summarized in Fig. 3a and indicate the driving force underlying
the emission changes. In agreement with previous findings (Liu et al.,
2016b), power plants are the primary component responsible for the decline in
NO<inline-formula><mml:math id="M131" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula>, and the associated bottom-up NO<inline-formula><mml:math id="M132" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions decreased by
59 % between 2011 and 2015. This finding was further supported by the
power plant emission trends shown afterwards in Sect. 3.3. The decrease in
both fitted and bottom-up emissions has accelerated since 2013 because of the
implementation of air pollution prevention and control action plans (the
State Council of China, 2013). Such plans require the deployment of
denitration devices for coal-fired boilers and cement precalciners, and the
requirements are not limited to power plants, as observed in earlier
policies. By 2015, 92 % of the power plant boilers and cement precalciner
kilns in China had installed denitration devices. In addition, low-efficiency
small coal-fired boilers and even complete factories have been phased out.
Iron, steel, and cement factories with an overall production capacity of 86,
44, and 263 Gg were shut down in China from 2013 to 2015. Additionally,
Chinese cities have pursued a reduction in coal consumption through the
gradual transformation of the energy system from coal to renewable energy and
natural gas. For instance, Beijing has outlined plans for “coal-free zones”
that ban coal usage, and these plans required the replacement of all
coal-fired boilers with natural gas in inner suburban districts by 2015
(Clean Air Action Plan 2013–2017, Beijing Municipal Government, 2013).
Accordingly, China reached peak coal consumption in 2013, and a decline of
4 % in coal consumption for the investigated cities was observed between
2013 and 2014 (Fig. 3b). Moreover, Chinese cities have been required to meet
more stringent vehicle emission standards. For instance, Euro IV emission
standards were widely implemented in 2015, and the NO<inline-formula><mml:math id="M133" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emission factor
is only 2.6 % of the Euro 0 standard for gasoline vehicles (Huo et al.,
2012). Because of the notable success of emission control induced by stricter
emission standards, the contributions of high-emitting old vehicles (Euro 0
in most cases) to overall emissions are becoming increasingly significant.
Reports have indicated that Euro 0 vehicles accounted for more than 50 %
of the total vehicle emissions in China in 2009 (MEP, 2010). Thus, China has
marked high-emitting vehicles with yellow labels, implemented traffic
restrictions and subsidized scrappage programs for these vehicles (Wu et al.,
2017). A total of 15 million yellow-label vehicles were scrapped between 2013
and 2015. Significant progress in controlling vehicle emissions has also been
observed with improvements in vehicular fuel combustion efficiency and
license registration control policies, which allocate quotas for new vehicles
through public auction or lottery. Note that all bottom-up inventories show
a lower increase rate around the year 2010, compared to the fitted emissions
(Fig. 3b). This is most likely caused by the spatial allocation approach
adopted in bottom-up inventories, which tends to diminish regional diversity
and may consequently result in smaller emission growth (see further
discussion in Sect. 3.2).</p>
</sec>
<sec id="Ch1.S3.SS2">
  <?xmltex \opttitle{Interannual trends of NO${}_{{x}}$ emissions for individual cities}?><title>Interannual trends of NO<inline-formula><mml:math id="M134" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions for individual cities</title>
      <p>The fitted results allowed for a closer examination of the trends and causes
of emission changes at the individual city level instead of at a regional
level, as performed in previous studies (e.g., Liu et al., 2016b). Figure 4
compares the fitted and bottom-up emissions for selected cities, which can
be considered in three broad categories: mega cities with large amount of
vehicle emissions (Guanzhou and Shanghai in Fig. 4a and b), cities with
power plants as the dominant emission source (Wuhai and Huainan in Fig. 4c
and d), and cities with industrial plants as the dominant emission source
(Karamay and Jiayuguan in Fig. 4e and f).</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F4" specific-use="star"><caption><p>Interannual trends in the fitted (gray squares) and bottom-up
anthropogenic NO<inline-formula><mml:math id="M135" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions for 2005 to 2015 including total (black
circles), industrial (pink circles), power plant (light blue circles), and
transportation (dark blue circles) emissions. Error bars denote the
uncertainty of the fitted NO<inline-formula><mml:math id="M136" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions. The IDs from Fig. 1 and the
correlation coefficients of the pair-wise trends between the bottom-up and
fitted NO<inline-formula><mml:math id="M137" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions are shown in the bracket after the name of the
city. Guangzhou<inline-formula><mml:math id="M138" display="inline"><mml:msup><mml:mi/><mml:mo>∗</mml:mo></mml:msup></mml:math></inline-formula> represents the cities of Guangzhou, Foshan, and
Dongguan, which are recognized as the same hot spot in the map of NO<inline-formula><mml:math id="M139" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula>
TVCDs.</p></caption>
          <?xmltex \igopts{width=312.980315pt}?><graphic xlink:href="https://acp.copernicus.org/articles/17/9261/2017/acp-17-9261-2017-f04.png"/>

        </fig>

      <?xmltex \floatpos{t}?><fig id="Ch1.F5" specific-use="star"><caption><p>Comparisons of the trends in satellite observations (left panels)
with those in the bottom-up emission inventory (right panels) at the province
(top panels) and city (bottom panels) level during 2005 to 2015. The box plots show the relative
changes in <bold>(a)</bold> the average OMI tropospheric NO<inline-formula><mml:math id="M140" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> column
densities for provinces in China; <bold>(b)</bold> the anthropogenic NO<inline-formula><mml:math id="M141" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula>
emissions for provinces in China; <bold>(c)</bold> the fitted NO<inline-formula><mml:math id="M142" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions
for cities investigated in this study; and <bold>(d)</bold> the anthropogenic
NO<inline-formula><mml:math id="M143" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions for the corresponding cities. The blue horizontal line is
the median of the relative differences; the red horizontal line is the mean
of the relative differences; the box denotes the 25 and 75 % percentiles;
and the whiskers denote the 10 and 90 % percentiles. The bottom-up
emission data are derived from the MEIC model.</p></caption>
          <?xmltex \igopts{width=312.980315pt}?><graphic xlink:href="https://acp.copernicus.org/articles/17/9261/2017/acp-17-9261-2017-f05.png"/>

        </fig>

      <p>Figure 4a and b show that megacities reached the emission peak prior to the
average timeline shown in Fig. 3. Here, we discuss in detail the temporal
variations in Guangzhou, the largest city in South China. The early decline
in emissions was primarily related to the stricter regulations on vehicles,
which was the only source that showed decreasing emissions, as indicated by
the bottom-up inventory. Guangzhou implemented Euro III emission standards
for all light-duty vehicles and heavy-duty diesel vehicles in 2006, which
was 2 years earlier than the national requirement. Traffic restrictions
for motorcycles and trucks and for yellow-label vehicles have also been
implemented since 2007 and 2008, respectively. In addition, alternative
fuels in buses and taxis have also been promoted in Guangzhou, and 75
and 94 % of these vehicles, respectively, were using liquefied petroleum
gas by 2009 (Zhang et al., 2013). The early decline before 2010 in Shanghai
shown in Fig. 4b is attributable to similarly strict regulations for vehicle
emissions that were implemented before the national schedule. In addition,
Guangzhou has gradually phased out the high-pollution iron and steel
industry since 2008; however, such emission reductions were not well
presented by the bottom-up inventory. In line with the national denitration
procedure, coal-fired power plants have remained a significant contributor
to emission reductions since 2011. The bottom-up NO<inline-formula><mml:math id="M144" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions from
power plants in Guangzhou decreased by over 50 % between 2011 and 2015,
because of the wider deployment of denitration devices at power plants.</p>
      <p>The interannual trends of NO<inline-formula><mml:math id="M145" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions for the cities of Wuhai and
Huainan are displayed in Fig. 4c and d, and power plants were the dominant
source of NO<inline-formula><mml:math id="M146" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions. Not surprisingly, the top-down and bottom-up
information was more consistent than the information for the other two
categories, because of the better quality of emission estimates for the
power sector. The fitted emissions decreased with the decline in emissions
from power plants around 2012, and this finding was related to the
deployment of denitration devices.</p>
      <p>Emission variations for cities for which the industrial sector was the
dominant emission source are shown in Fig. 4e and f, which indicate
significant inconsistencies in the top-down and bottom-up information, even
for the total amount. Cities belonging to this category were usually medium
and small cities. For instance, the city of Jiayuguan (Fig. 4f) has a total
population of 0.2 million, a vehicle population of 0.03 million and a
large-sized industrial enterprise (Jiuquan Iron &amp; Steel (Group) Co.,
Ltd). Industrial activities are the most likely contributor to the recent
deceleration and even decline in total emissions, because of the small human
and vehicle populations and the limited amount of power plant emissions
(light blue line) in the city. To meet the demands of the air pollution
prevention and control action plan (the State Council of China, 2013), the
iron and steel enterprises have been required to regulate their emissions
since 2013. Additionally, the city is required to meet stricter vehicle
emission standards and retire aged vehicles. However, the bottom-up
inventory for the city of Jiayuguan was consistent with this analysis for
only the transportation sector and not the industrial sector as shown in
Fig. 4f. The bottom-up transportation emissions experienced a decline of
10 % and a sharp increase of 20 % in the vehicle population between 2013
and 2015. In addition, the NO<inline-formula><mml:math id="M147" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions from the industrial sector
were fairly steady and showed a decrease of only 2 % between 2013 and 2015
and account for a small share (20 %) of the total emissions. For
industrial emissions, MEIC first downscaled provincial totals to counties
using industrial GDP, and then allocate county emissions to grids with
population density. Thus, uncertainty of emissions from the industrial sector
is larger than that from power plants. Such changes in the industrial sector
most probably represent the regional average level and do not represent the
levels for a city with a large-sized iron and steel enterprise, because of
the uncertainty of downscaling approaches adopted in the bottom-up
inventory.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F6" specific-use="star"><caption><p><bold>(a)</bold> Correlation coefficients of the pair-wise trends
between the bottom-up anthropogenic and fitted NO<inline-formula><mml:math id="M148" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions for all
selected sites during 2006<inline-formula><mml:math id="M149" display="inline"><mml:msup><mml:mi/><mml:mo>∗</mml:mo></mml:msup></mml:math></inline-formula> to 2014<inline-formula><mml:math id="M150" display="inline"><mml:msup><mml:mi/><mml:mo>∗</mml:mo></mml:msup></mml:math></inline-formula>. The results for sites
with correlation coefficients less than <inline-formula><mml:math id="M151" display="inline"><mml:mo>-</mml:mo></mml:math></inline-formula>0.4 or larger than 0.9 are
indicated by digits. <bold>(b)</bold> Scatter plots of the fitted NO<inline-formula><mml:math id="M152" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula>
emissions for investigated cities versus bottom-up anthropogenic emission
inventories during 2006<inline-formula><mml:math id="M153" display="inline"><mml:msup><mml:mi/><mml:mo>∗</mml:mo></mml:msup></mml:math></inline-formula> to 2014<inline-formula><mml:math id="M154" display="inline"><mml:msup><mml:mi/><mml:mo>∗</mml:mo></mml:msup></mml:math></inline-formula>. Urban emissions from
bottom-up inventories are integrated over an area of 40 km <inline-formula><mml:math id="M155" display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 40 km
(see Sect. 2.2). Results with correlation coefficients less than <inline-formula><mml:math id="M156" display="inline"><mml:mo>-</mml:mo></mml:math></inline-formula>0.4 or
larger than 0.9 are color coded by gray and green, respectively.</p></caption>
          <?xmltex \igopts{width=369.885827pt}?><graphic xlink:href="https://acp.copernicus.org/articles/17/9261/2017/acp-17-9261-2017-f06.png"/>

        </fig>

      <p>Although we used bottom-up inventories to interpret the changes in NO<inline-formula><mml:math id="M157" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula>
emission, certain notable discrepancies occurred between the fitted
emissions and the bottom-up inventories. We further explored the reasons for
these inconsistencies in cities by examining the differences in trends
between top-down and bottom-up estimates at different spatial scales. Figure 5
presents the temporal variations at provincial and city scales from
2006<inline-formula><mml:math id="M158" display="inline"><mml:msup><mml:mi/><mml:mo>∗</mml:mo></mml:msup></mml:math></inline-formula> to 2014<inline-formula><mml:math id="M159" display="inline"><mml:msup><mml:mi/><mml:mo>∗</mml:mo></mml:msup></mml:math></inline-formula> for the top-down and bottom-up data sets.
The top-down information at the provincial level (Fig. 5a) was the 3-year
average OMI NO<inline-formula><mml:math id="M160" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> column densities for non-background regions, where the
average annual NO<inline-formula><mml:math id="M161" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> column densities were larger than <inline-formula><mml:math id="M162" 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> molec cm<inline-formula><mml:math id="M163" 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> or the average NO<inline-formula><mml:math id="M164" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> column densities for summer
exceeded those for winter in Liu et al. (2016b), and the top-down estimates
(Fig. 5c) at the city level were derived from this study. The bottom-up
emissions were calculated by summing the emissions of the corresponding
grids belonging to individual provinces (Fig. 5b) or cities (Fig. 5d, see
Sect. 2.2). Not surprisingly, the comparison of the two independent data
sets showed that the trends at both the provincial and city levels were
generally consistent, with both levels experiencing a sharp rise before
2012<inline-formula><mml:math id="M165" display="inline"><mml:msup><mml:mi/><mml:mo>∗</mml:mo></mml:msup></mml:math></inline-formula> (2011<inline-formula><mml:math id="M166" display="inline"><mml:msup><mml:mi/><mml:mo>∗</mml:mo></mml:msup></mml:math></inline-formula> in Fig. 5c) and a continuous decline
thereafter. However, a closer examination of the magnitude of relative
changes showed that the differences were scale dependent. The
provincial-level comparison showed a growth trend of 40 % <inline-formula><mml:math id="M167" display="inline"><mml:mo>±</mml:mo></mml:math></inline-formula> 26 %
and 34 % <inline-formula><mml:math id="M168" display="inline"><mml:mo>±</mml:mo></mml:math></inline-formula> 21 % from 2006<inline-formula><mml:math id="M169" display="inline"><mml:msup><mml:mi/><mml:mo>∗</mml:mo></mml:msup></mml:math></inline-formula> to 2012<inline-formula><mml:math id="M170" display="inline"><mml:msup><mml:mi/><mml:mo>∗</mml:mo></mml:msup></mml:math></inline-formula> and a
subsequent declining trend of 9 % <inline-formula><mml:math id="M171" display="inline"><mml:mo>±</mml:mo></mml:math></inline-formula> 4 % and 14 % <inline-formula><mml:math id="M172" display="inline"><mml:mo>±</mml:mo></mml:math></inline-formula> 6 %
from 2012<inline-formula><mml:math id="M173" display="inline"><mml:msup><mml:mi/><mml:mo>∗</mml:mo></mml:msup></mml:math></inline-formula> to 2014<inline-formula><mml:math id="M174" display="inline"><mml:msup><mml:mi/><mml:mo>∗</mml:mo></mml:msup></mml:math></inline-formula> for the top-down and bottom-up data
sets, respectively, and indicated the acceptable accuracy of provincial
totals in bottom-up estimates. However, the city-level comparison exhibited
a large discrepancy in the magnitude of change rates. For instance, the
top-down growth rates reached 45 % <inline-formula><mml:math id="M175" display="inline"><mml:mo>±</mml:mo></mml:math></inline-formula> 46 % in the period from
2006<inline-formula><mml:math id="M176" display="inline"><mml:msup><mml:mi/><mml:mo>∗</mml:mo></mml:msup></mml:math></inline-formula> to 2012<inline-formula><mml:math id="M177" display="inline"><mml:msup><mml:mi/><mml:mo>∗</mml:mo></mml:msup></mml:math></inline-formula>, whereas the bottom-up rates were only
25 % <inline-formula><mml:math id="M178" display="inline"><mml:mo>±</mml:mo></mml:math></inline-formula> 27 % for the same period.</p>
      <p>We expect that the scale dependence of the differences shown in Fig. 5 may
be explained by the spatial allocation approach adopted in bottom-up
inventories. Current gridded bottom-up emission inventories rely heavily on
spatial proxies because rare emissions, excluding the emissions from stacks
of large point sources, can be directly measured. A variety of spatial
proxies, such as population density, road density, and satellite-observed
nightlights, are used to geographically distribute emission totals from a
large scale down to the scale of geographic grids of various sizes. Several
studies (e.g., Hogue et al., 2016) have indicated that such a spatial
distribution approach using proxy data introduces significant uncertainties
because emissions can be misallocated spatially and temporally. Although the
MEIC inventory has substantially improved its accuracy, such as by using the
high-resolution power plant database CPED (Liu et al., 2015), a lack of data
has led to the inclusion of other types of point sources (such as industrial
boilers) as areal sources of emissions. For example, the MEIC first
downscales provincial industrial emission totals to county totals according
to industrial GDP values and then distributes county emissions to grids
according to the population density. However, industrial facility locations
are likely to be decoupled from spatial proxies, because polluted facilities
are often required to be located in rural areas with smaller GDP and
populations (Zheng et al., 2017), and this decoupling may have resulted in
the underestimation of emissions from steel and iron factories shown in Fig. 4f.
In addition, the spatial distribution of proxies cannot easily represent
the emission changes caused by anti-leapfrogging policies implemented in
cities ahead of the national schedule, such as the previously discussed new
vehicle emission standards in Guangzhou. Thus, regional diversity may have
been diminished and consequently resulted in the small standard deviation
over cities shown in Fig. 5d.</p>
      <p>The correlation coefficients of the pair-wise trends between the fitted
NO<inline-formula><mml:math id="M179" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions and the bottom-up inventory for the period 2006<inline-formula><mml:math id="M180" display="inline"><mml:msup><mml:mi/><mml:mo>∗</mml:mo></mml:msup></mml:math></inline-formula>
to 2014<inline-formula><mml:math id="M181" display="inline"><mml:msup><mml:mi/><mml:mo>∗</mml:mo></mml:msup></mml:math></inline-formula> are illustrated in Fig. 6. The correlation coefficient of
the time series of NO<inline-formula><mml:math id="M182" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions showed remarkable diversity for cities
and reached over 0.9 for Urumqi (no. 9 in Fig. 6) and dropped to less than
<inline-formula><mml:math id="M183" display="inline"><mml:mo>-</mml:mo></mml:math></inline-formula>0.7 for Jinzhou (no. 5 in Fig. 6), probably because of the high
uncertainties of the bottom-up inventories for cities. Notably, the negative
correlation coefficients do not necessarily correspond to a strong inverse
linear relationship and may suggest inconsistency over only one or two
periods (Fig. 4b). Additionally, the negative correlation coefficients were
always observed when the time series of fitted emissions experienced a minor
fluctuation without a significant trend, as demonstrated in Fig. 6b by
cities with a correlation coefficient less than <inline-formula><mml:math id="M184" display="inline"><mml:mo>-</mml:mo></mml:math></inline-formula>0.4.</p>
</sec>
<sec id="Ch1.S3.SS3">
  <?xmltex \opttitle{Interannual trends in OMI NO${}_{{x}}$ emissions for power plants}?><title>Interannual trends in OMI NO<inline-formula><mml:math id="M185" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions for power plants</title>
      <p>The trends in fitted NO<inline-formula><mml:math id="M186" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions for seven power plants from 2006<inline-formula><mml:math id="M187" display="inline"><mml:msup><mml:mi/><mml:mo>∗</mml:mo></mml:msup></mml:math></inline-formula> to 2014<inline-formula><mml:math id="M188" display="inline"><mml:msup><mml:mi/><mml:mo>∗</mml:mo></mml:msup></mml:math></inline-formula> are shown in Fig. 7. The changes in the total NO<inline-formula><mml:math id="M189" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula>
mass and derived NO<inline-formula><mml:math id="M190" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions were consistent with the addition of new
units in individual power plants until the installation of denitration
devices. The dramatic growth in NO<inline-formula><mml:math id="M191" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions (red line) prior to
2010<inline-formula><mml:math id="M192" display="inline"><mml:msup><mml:mi/><mml:mo>∗</mml:mo></mml:msup></mml:math></inline-formula>, which reached 89 % on average for all power plants
investigated in this study, was driven by increases in the capacity of
84 % for the corresponding power plants (gray bar). However, the
subsequent decline in NO<inline-formula><mml:math id="M193" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions could not be explained by the
simultaneous changes in total unit capacities, which increased by 3 % from
2010<inline-formula><mml:math id="M194" display="inline"><mml:msup><mml:mi/><mml:mo>∗</mml:mo></mml:msup></mml:math></inline-formula> to 2014<inline-formula><mml:math id="M195" display="inline"><mml:msup><mml:mi/><mml:mo>∗</mml:mo></mml:msup></mml:math></inline-formula>, but suggests a good agreement with the
wider deployment of denitration devices, such as SCR equipment. The
installation of SCR devices generally ensures a NO<inline-formula><mml:math id="M196" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> removal efficiency
of 80–85 % (Forzatti et al., 2001). However, the denitration devices used
in Chinese power plants usually do not meet this standard efficiency,
because of the non-optimal use of catalysts and reductants. The average
removal efficiency of SCR equipment for 2014 was only 60 % on the basis of
statistics from the CPED. In this way, the increasing penetration of SCR
equipment (up to 73 %, blue line) corresponded to a decrease of
approximately 40 % (i.e., 73 % <inline-formula><mml:math id="M197" display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 60 %) in NO<inline-formula><mml:math id="M198" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions,
a result consistent with the changes in fitted emissions. The fitted
emissions were further compared with the bottom-up emission estimates, and
both values shared a similar trend. The significant decline of 40 <inline-formula><mml:math id="M199" display="inline"><mml:mo>±</mml:mo></mml:math></inline-formula> 22 %
(mean <inline-formula><mml:math id="M200" display="inline"><mml:mo>±</mml:mo></mml:math></inline-formula> standard deviation) in fitted NO<inline-formula><mml:math id="M201" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions for
individual power plants from 2010<inline-formula><mml:math id="M202" display="inline"><mml:msup><mml:mi/><mml:mo>∗</mml:mo></mml:msup></mml:math></inline-formula> to 2014<inline-formula><mml:math id="M203" display="inline"><mml:msup><mml:mi/><mml:mo>∗</mml:mo></mml:msup></mml:math></inline-formula> was generally
consistent with the simultaneous decline in bottom-up estimates of <inline-formula><mml:math id="M204" display="inline"><mml:mrow><mml:mn mathvariant="normal">22</mml:mn><mml:mo>±</mml:mo><mml:mn mathvariant="normal">29</mml:mn></mml:mrow></mml:math></inline-formula> %. However, a minor difference in the peak year of emissions
was detected for a few power plants, and was most probably caused by
uncertainty in the fitted emissions related to the lack of interannual
variations in NO<inline-formula><mml:math id="M205" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> lifetimes.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F7"><caption><p>Interannual trends of the fitted (red line) and bottom-up NO<inline-formula><mml:math id="M206" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula>
emissions for selected power plants during 2005 to 2015. The emissions
deriving from the MEIC and REAS v2.1 inventory are displayed in pink and
green, respectively. The bar denotes the total capacity of selected power
plants. The blue line denotes the penetration of power plants with
denitration devices (defined as the percentage of unit capacity of power
plants installing SCR in the total capacity of all the power plants). Error
bars show the uncertainties for fitted emissions by this method (see
Sect. 3.4).</p></caption>
          <?xmltex \igopts{width=236.157874pt}?><graphic xlink:href="https://acp.copernicus.org/articles/17/9261/2017/acp-17-9261-2017-f07.png"/>

        </fig>

      <p>China has implemented the new emission standards for thermal power plants
(Ministry of Environmental Protection of China (MEP), 2011) in 2012,
requiring power plants, particularly large plants, to install denitration
devices, such as SCR equipment, to control their NO<inline-formula><mml:math id="M207" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions. The
deployment of denitration devices (shown in Fig. 7) was consistent with this
new policy, and the national average penetration of SCR equipment grew from
18 to 86 % between 2011 and 2015 (China Electricity Council,
2012–2016). Given that the overall capacity of the power plants
investigated in this study was equivalent to only 2 % of the total
national capacity, we may not be able to conclude that the temporal variations
in NO<inline-formula><mml:math id="M208" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions derived from the seven power plants reflect the emissions
from large power plants at the national level. While for the investigated
power plants, the derived emissions were consistent with the bottom-up
emissions and the time series of the two estimates were well correlated,
even for mountainous sites where the absolute values of the emission
estimates differed significantly (Fig. 6a). The good consistency increased
our confidence that the fitted emission trends accurately represented the
real-world emission variations, because the uncertainty of the bottom-up
emission inventory for power plants is fairly low (Liu et al., 2015).</p>
</sec>
<sec id="Ch1.S3.SS4">
  <title>Uncertainties</title>
      <p>The fitted NO<inline-formula><mml:math id="M209" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions were compared with the bottom-up emission
estimates (Sect. 2.2) for all 48 cities and seven power plants in Fig. 8, and
their correlations were consistent with the average emission estimates for
multiple years shown in previous work (Liu et al., 2016a). In general,
the comparisons indicated consistency among non-mountainous sites, which
presented a higher correlation coefficient for power plants (blue symbols in
Fig. 8a, <inline-formula><mml:math id="M210" display="inline"><mml:mrow><mml:mi>r</mml:mi><mml:mo>=</mml:mo><mml:mn mathvariant="normal">0.89</mml:mn></mml:mrow></mml:math></inline-formula>) than cities (blue symbols in Fig. 8b, <inline-formula><mml:math id="M211" display="inline"><mml:mrow><mml:mi>r</mml:mi><mml:mo>=</mml:mo><mml:mn mathvariant="normal">0.81</mml:mn></mml:mrow></mml:math></inline-formula>). The
results for the mountainous sites showed higher scatter for both power
plants (red symbols in Fig. 8a, <inline-formula><mml:math id="M212" display="inline"><mml:mrow><mml:mi>r</mml:mi><mml:mo>=</mml:mo><mml:mn mathvariant="normal">0.79</mml:mn></mml:mrow></mml:math></inline-formula>) and cities (red symbols in Fig. 8b,
<inline-formula><mml:math id="M213" display="inline"><mml:mrow><mml:mi>r</mml:mi><mml:mo>=</mml:mo><mml:mn mathvariant="normal">0.44</mml:mn></mml:mrow></mml:math></inline-formula>), thus confirming that those top-down estimates had higher
uncertainties because of inaccurate ECMWF wind fields for mountainous sites
(Liu et al., 2016a). The comparable correlation among the results presented
here and in the previous study by Liu et al. (2016a) increased our confidence
in the accuracy of the fitted results.</p>
      <p>We estimated the uncertainty of the fitted NO<inline-formula><mml:math id="M214" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions and their
trends by using a method analogous to that in Liu et al. (2016a) because of
the consistency in methodology between the two studies. The uncertainty
analysis was performed on the basis of the fit performance and according to
sensitivity studies that have investigated the dependencies on a priori
settings, which are detailed in the supplement of Liu et al. (2016a). The
major sources of errors contributing to the overall uncertainties included
(a) fit error, (b) choice of fit intervals, (c) tropospheric NO<inline-formula><mml:math id="M215" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> VCDs
and the NO<inline-formula><mml:math id="M216" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> <inline-formula><mml:math id="M217" display="inline"><mml:mo>/</mml:mo></mml:math></inline-formula> NO<inline-formula><mml:math id="M218" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> ratio, (d) choice of wind fields and (e) lifetime
variations. The uncertainties arising from (a) to (c) were consistent with
those reported in Liu et al. (2016a). Here, we briefly discuss the impact of
(d) and (e).</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F8" specific-use="star"><caption><p>Scatter plots of the fitted NO<inline-formula><mml:math id="M219" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions for the investigated
<bold>(a)</bold> power plants and <bold>(b)</bold> cities versus the bottom-up
emission inventories during 2006<inline-formula><mml:math id="M220" display="inline"><mml:msup><mml:mi/><mml:mo>∗</mml:mo></mml:msup></mml:math></inline-formula> to 2014<inline-formula><mml:math id="M221" display="inline"><mml:msup><mml:mi/><mml:mo>∗</mml:mo></mml:msup></mml:math></inline-formula>. Urban emissions
from bottom-up inventories are integrated over an area of
40 km <inline-formula><mml:math id="M222" display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 40 km (see Sect. 2.2). The correlation coefficients of
non-mountainous sites for individual 3-year periods are shown in brackets.
Open circles represent the average emissions for non-mountainous (blue) and
mountainous (red) sites during the entire period. The correlation
coefficients of the average emissions for non-mountainous and mountainous
sites are color-coded in blue and red, respectively. The straight line
represents the ratio of <inline-formula><mml:math id="M223" display="inline"><mml:mrow><mml:mn mathvariant="normal">1</mml:mn><mml:mo>:</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:math></inline-formula>.</p></caption>
          <?xmltex \igopts{width=398.338583pt}?><graphic xlink:href="https://acp.copernicus.org/articles/17/9261/2017/acp-17-9261-2017-f08.png"/>

        </fig>

      <p>(d) Choice of wind fields. The NO<inline-formula><mml:math id="M224" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> trends observed under weak-wind
conditions may vary from those under all-wind conditions (Lu et al., 2015),
because higher wind speeds are expected to cause longer NO<inline-formula><mml:math id="M225" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> lifetimes
because of the faster dilution of NO<inline-formula><mml:math id="M226" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> (Valin et al., 2013). A change in
the weak-wind conditions by all-wind conditions affects the resulting total
mass by approximately 10 % on average.</p>
      <p>(e) Lifetime variations. We use multiple-year average lifetimes and 3-year
average NO<inline-formula><mml:math id="M227" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> masses to calculate NO<inline-formula><mml:math id="M228" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions trends in this study.
The variations in total NO<inline-formula><mml:math id="M229" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> mass do not necessarily correlate linearly
with NO<inline-formula><mml:math id="M230" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions, because of potential changes in the NO<inline-formula><mml:math id="M231" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> lifetimes related to variations in
meteorology and NO<inline-formula><mml:math id="M232" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> chemistry. However, the temporal variations in
lifetimes corresponding to the 3-year moving averages of TVCDs are reduced
significantly, as supported by the similar decreases in the 3-year mean
NO<inline-formula><mml:math id="M233" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions and OMI NO<inline-formula><mml:math id="M234" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> observations over urban areas in the US
(Lu et al., 2015). In addition, we could not unambiguously relate the
variability of fitted NO<inline-formula><mml:math id="M235" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> lifetimes to NO<inline-formula><mml:math id="M236" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> levels (Liu et al.,
2016a).</p>
      <p>The method was applied to the period prior to the row anomaly (the 3-year
period from 2005 to 2007), which had a larger number of observations than
the other periods. The method was successful for 19 sites, and the fitted
lifetimes were not sensitive to the NO<inline-formula><mml:math id="M237" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> changes within the studied
period, with the lifetimes increasing by only 9 % when the average
NO<inline-formula><mml:math id="M238" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> increased by <inline-formula><mml:math id="M239" display="inline"><mml:mo>∼</mml:mo></mml:math></inline-formula> 20 % compared with the multiple-year
level. The uncertainties caused by lifetime variations were estimated to be
10 %, and this value was applied to all considered sources.</p>
      <p>The total uncertainty was defined as the root of the quadratic sum of the
aforementioned contributions, which were assumed to be independent. We
estimated that the total uncertainties of the fitted NO<inline-formula><mml:math id="M240" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions were
within 66–99 % for all investigated sites. Notably, this estimate is
rather conservative because of the assumption that all the contributors to
uncertainties are independent. In addition, the uncertainty in emission
trends was significantly lower than that of emissions because the errors
from the choice of fit intervals, wind fields, tropospheric columns, and
NO<inline-formula><mml:math id="M241" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> <inline-formula><mml:math id="M242" display="inline"><mml:mo>/</mml:mo></mml:math></inline-formula> NO<inline-formula><mml:math id="M243" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> ratios were generally compensated for in the assessment of
trends.</p>
</sec>
</sec>
<sec id="Ch1.S4" sec-type="conclusions">
  <title>Conclusions</title>
      <p>We quantified the NO<inline-formula><mml:math id="M244" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions of cities over China obtained from
satellite NO<inline-formula><mml:math id="M245" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> observations for the period 2005 to 2015. The lifetimes
were determined from the average changes in NO<inline-formula><mml:math id="M246" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> distributions under
windy conditions compared with calm conditions, and the emissions were
subsequently estimated by dividing the total mass of NO<inline-formula><mml:math id="M247" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> integrated
around the source of interest in any 3 consecutive years from 2005 to
2015 by the derived lifetimes. The method was successfully applied to 48
cities and seven power plants to obtain the NO<inline-formula><mml:math id="M248" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emission trends over China.</p>
      <p>We detected similar temporal variations in the derived NO<inline-formula><mml:math id="M249" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions
for cities and power plants, both of which experienced a rapid growth until
approximately 2011 and a sharp decline thereafter. The NO<inline-formula><mml:math id="M250" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions
from selected cities experienced an average growth of 52 % prior to
2011<inline-formula><mml:math id="M251" display="inline"><mml:msup><mml:mi/><mml:mo>∗</mml:mo></mml:msup></mml:math></inline-formula>, because of the increase in fuel consumption. The subsequent
decline of 21 % was quantitatively attributed to the successful control of
NO<inline-formula><mml:math id="M252" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions in the power, industrial and transportation sectors. In
addition to installing denitration devices at power plants and cement
plants, China has transformed its industrial structure by phasing out
heavily polluting industrial factories, decreasing coal consumption,
controlling vehicle emissions through stricter emission standards and
scrapping aged vehicles. The average emission trend fitted by this study is
consistent with the previous findings, which showed that OMI NO<inline-formula><mml:math id="M253" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> levels
peaked in 2011 over China (Krotkov et al., 2016; Duncan et al., 2016) and
NO<inline-formula><mml:math id="M254" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions from satellite data assimilation peaked in 2011/2012
(Miyazaki et al., 2017; van der A et al., 2017; Souri et al., 2017),
respectively. Additionally, the fitted emission peaks for individual cities
showed reasonable agreement with the peaks of OMI NO<inline-formula><mml:math id="M255" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> levels at
provincial level (Liu et al., 2016b). Half of the investigated cities
reached simultaneous emission peaks with the corresponding provinces. For
the other half, the majority (over 70 %) reached emission peaks prior to
the average provincial timeline, which are most likely caused by emission
control policies implemented in the city ahead of the provincial schedule,
such as the previously discussed new vehicle emission standards in
Guangzhou.</p>
      <p>We further compared the derived NO<inline-formula><mml:math id="M256" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions with the bottom-up
emission estimates for individual cities. Megacities with a large amount of
vehicle emissions reached the emission peak prior to the average timeline,
because of the stricter vehicle regulations that were implemented ahead of
the national schedule. Cities with power and industrial sectors as the
dominant emission sources reached the emission peak at dates that were
consistent with the schedule for emission control in the corresponding
sectors. In addition, we found that the derived NO<inline-formula><mml:math id="M257" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions were
significantly less consistent with the regional inventory MEIC for cities
(<inline-formula><mml:math id="M258" display="inline"><mml:mrow><mml:mi>r</mml:mi><mml:mo>=</mml:mo><mml:mn mathvariant="normal">0.4</mml:mn></mml:mrow></mml:math></inline-formula> on average) than the high-resolution power plant inventory CPED, a
result related to the uncertainties in the spatial allocation technique, in
which surrogates were used to break down regional-based emission data to the
level of cities. However, the discrepancy was strongly scale dependent, and
the trends between the top-down and bottom-up estimates were consistent at
the province level but not at the city level. This finding indicated that
the allocation technique used in bottom-up inventory misrepresents the
spatial and temporal patterns for emissions over cities.</p>
      <p>Our results indicated that OMI NO<inline-formula><mml:math id="M259" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> observations can be used to estimate
NO<inline-formula><mml:math id="M260" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emission trends for individual cities and power plants, even those
with a polluted background. Moreover, this method can be applied to quantify
the emission variations from various hot spots worldwide. Notably, the
lifetimes were derived on the basis of the average NO<inline-formula><mml:math id="M261" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> columns for the
entire study period of 2005–2015 because of a lack of statistics for
shorter periods. Because future satellite instruments, such as TROPOMI
(Veefkind et al., 2012), GEMS (Kim et al., 2012), TEMPO (Chance et al.,
2012), and Sentinel-4 (Ingmann et al., 2012), have improved spatial and
temporal resolution, the capabilities of this method is expected to be
further enhanced. We expect that future estimates of interannual lifetimes
as well as diurnal cycles from geostationary satellites will be able to
account for changes in meteorology and NO<inline-formula><mml:math id="M262" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> chemistry. In addition, the
trend analysis for annual and even seasonal NO<inline-formula><mml:math id="M263" display="inline"><mml:msub><mml:mi/><mml:mi>x</mml:mi></mml:msub></mml:math></inline-formula> emissions should be
achievable and should serve as a more reliable tool for interpreting
emission changes.</p>
</sec>

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

      <p>The OMI tropospheric NO<inline-formula><mml:math id="M264" display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> (DOMINO) v2.0 product can be
downloaded from <uri>http://www.temis.nl/airpollution/no2.html</uri> (Boersma et
al., 2011). The Emission Database for Global Atmospheric Research version 4.3
(EDGAR v4.3) can be obtained from
<uri>http://edgar.jrc.ec.europa.eu/overview.php?v=431</uri>. The Regional Emission
inventory in Asia version 2.1 (REAS v2.1) is available from
<uri>https://www.nies.go.jp/REAS/</uri>. The Multi-resolution Emission Inventory
for China (MEIC) is available from <uri>http://www.meicmodel.org</uri>.
We thank the two anonymous reviewers for helpful comments during ACP
discussions.</p>
  </notes><app-group>
        <supplementary-material position="anchor"><p><bold>The Supplement related to this article is available online at <inline-supplementary-material xlink:href="https://doi.org/10.5194/acp-17-9261-2017-supplement" xlink:title="pdf">https://doi.org/10.5194/acp-17-9261-2017-supplement</inline-supplementary-material>.</bold></p></supplementary-material>
        </app-group><notes notes-type="competinginterests">

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

      <p>This article is part of the special issue “Ten years of Ozone
Monitoring Instrument (OMI) observations (ACP/AMT inter-journal SI)”. It
is not associated with a conference.</p>
  </notes><ack><title>Acknowledgements</title><p>This research was funded by the National Natural Science Foundation of China
(41625020, 41571130032), the National Key R&amp;D Program (2016YFC0201506),
China's National Basic Research Program (2014CB441301), and the MarcoPolo
project of the European Union Seventh Framework Programme (FP7/2007-2013)
under grant agreement number 606953.<?xmltex \hack{\newline}?><?xmltex \hack{\newline}?>The
article processing charges for this open-access <?xmltex \hack{\newline}?> publication
were covered by the Max Planck Society.<?xmltex \hack{\newline}?><?xmltex \hack{\newline}?> Edited
by: Gerrit de Leeuw<?xmltex \hack{\newline}?> Reviewed by: two anonymous referees</p></ack><?xmltex \hack{\newpage}?><?xmltex \hack{\newpage}?><ref-list>
    <title>References</title>

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    </app></app-group></back>
    <!--<article-title-html>NO<sub><i>x</i></sub> emission trends over Chinese cities estimated from OMI observations during 2005 to 2015</article-title-html>
<abstract-html><p class="p">Satellite nitrogen dioxide (NO<sub>2</sub>) observations have been widely used to
evaluate emission changes. To determine trends in nitrogen oxides (NO<sub><i>x</i></sub>)
emission over China, we used a method independent of chemical transport
models to quantify the NO<sub><i>x</i></sub> emissions from 48 cities and seven power
plants over China, on the basis of Ozone Monitoring Instrument (OMI) NO<sub>2</sub>
observations from 2005 to 2015. We found that NO<sub><i>x</i></sub> emissions over 48
Chinese cities increased by 52 % from 2005 to 2011 and decreased by
21 % from 2011 to 2015. The decrease since 2011 could be mainly
attributed to emission control measures in power sector; while cities with
different dominant emission sources (i.e., power, industrial, and
transportation sectors) showed variable emission decline timelines that
corresponded to the schedules for emission control in different sectors. The
time series of the derived NO<sub><i>x</i></sub> emissions was consistent with the
bottom-up emission inventories for all power plants (<i>r</i> = 0. 8 on average), but
not for some cities (<i>r</i> = 0. 4 on average). The lack of consistency observed
for cities was most probably due to the high uncertainty of bottom-up urban
emissions used in this study, which were derived from downscaling the
regional-based emission data to city level by using spatial distribution proxies.</p></abstract-html>
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