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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" xml:lang="en" dtd-version="3.0" article-type="research-article"><?xmltex \bartext{Research article}?>
  <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-22-2221-2022</article-id><title-group><article-title>Development and application of a street-level meteorology and pollutant tracking system (S-TRACK)</article-title><alt-title>Development and application of S-TRACK</alt-title>
      </title-group><?xmltex \runningtitle{Development and application of S-TRACK}?><?xmltex \runningauthor{H. Zhang et al.}?>
      <contrib-group>
        <contrib contrib-type="author" corresp="no" rid="aff1">
          <name><surname>Zhang</surname><given-names>Huan</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="yes" rid="aff1">
          <name><surname>Gong</surname><given-names>Sunling</given-names></name>
          <email>gongsl@cma.gov.cn</email>
        </contrib>
        <contrib contrib-type="author" corresp="yes" rid="aff1">
          <name><surname>Zhang</surname><given-names>Lei</given-names></name>
          <email>leiz09@cma.gov.cn</email>
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff2">
          <name><surname>Ni</surname><given-names>Jingwei</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff1">
          <name><surname>He</surname><given-names>Jianjun</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff1">
          <name><surname>Wang</surname><given-names>Yaqiang</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff3">
          <name><surname>Wang</surname><given-names>Xu</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff4">
          <name><surname>Shi</surname><given-names>Lixin</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff1">
          <name><surname>Mo</surname><given-names>Jingyue</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff1">
          <name><surname>Ke</surname><given-names>Huabing</given-names></name>
          
        <ext-link>https://orcid.org/0000-0002-0552-7026</ext-link></contrib>
        <contrib contrib-type="author" corresp="no" rid="aff1">
          <name><surname>Lu</surname><given-names>Shuhua</given-names></name>
          
        </contrib>
        <aff id="aff1"><label>1</label><institution>State Key Laboratory of Severe Weather &amp; Key Laboratory of Atmospheric Chemistry of CMA, <?xmltex \hack{\break}?> Chinese Academy of Meteorological Sciences, Beijing 100081, China</institution>
        </aff>
        <aff id="aff2"><label>2</label><institution>Henan Tianlang Ecological Technology Co. Ltd., Zhengzhou 450000, China</institution>
        </aff>
        <aff id="aff3"><label>3</label><institution>Hangzhou Yizhang Technology Co., Ltd., Hangzhou 310000, China</institution>
        </aff>
        <aff id="aff4"><label>4</label><institution>Key Laboratory of Meteorology and Ecological Environment of Hebei Province, Shijiazhuang 050000, China</institution>
        </aff>
      </contrib-group>
      <author-notes><corresp id="corr1">Sunling Gong (gongsl@cma.gov.cn) and Lei Zhang (leiz09@cma.gov.cn)</corresp></author-notes><pub-date><day>17</day><month>February</month><year>2022</year></pub-date>
      
      <volume>22</volume>
      <issue>4</issue>
      <fpage>2221</fpage><lpage>2236</lpage>
      <history>
        <date date-type="received"><day>26</day><month>August</month><year>2021</year></date>
           <date date-type="accepted"><day>17</day><month>January</month><year>2022</year></date>
           <date date-type="rev-recd"><day>12</day><month>January</month><year>2022</year></date>
           <date date-type="rev-request"><day>3</day><month>September</month><year>2021</year></date>
      </history>
      <permissions>
        <copyright-statement>Copyright: © 2022 </copyright-statement>
        <copyright-year>2022</copyright-year>
      <license license-type="open-access"><license-p>This work is licensed under the Creative Commons Attribution 4.0 International License. To view a copy of this licence, visit <ext-link ext-link-type="uri" xlink:href="https://creativecommons.org/licenses/by/4.0/">https://creativecommons.org/licenses/by/4.0/</ext-link></license-p></license></permissions><self-uri xlink:href="https://acp.copernicus.org/articles/.html">This article is available from https://acp.copernicus.org/articles/.html</self-uri><self-uri xlink:href="https://acp.copernicus.org/articles/.pdf">The full text article is available as a PDF file from https://acp.copernicus.org/articles/.pdf</self-uri>
      <abstract><title>Abstract</title>

      <p id="d1e198">A multi-model simulation system for street-level
circulation and pollutant tracking (S-TRACK) has been developed by
integrating the Weather Research and Forecasting (WRF), the STAR-CCM+
(computational fluid dynamics model – CFD), and the Flexible Particle
(FLEXPART) models. The winter wind environmental characteristics and the
potential contribution of traffic sources to nearby receptor sites in a city
district of China are analysed with the system for January 2019. It is found
that complex building layouts change the structure of the wind field and
thus have an impact on the transport of pollutants. The wind speed inside
the building block is lower than the background wind speed due to the
dragging effect of dense buildings. Ventilation is better when the dominant
airflow is in the same direction as the building layout. Influenced by the
building layout, the local circulations show that the windward side of the
building is mostly the divergence zone, and the leeward side is mostly the
convergence zone, which is more obvious for high buildings. With the
hypothesis that the traffic sources are uniformly distributed on each road
and with identical traffic intensity, the potential contribution ratios
(PCRs) of four traffic sources to certain specific sites under the influence
of the street-level circulations are estimated with the method of residence
time analysis. It is found that the contribution ratio varies with the
height of the receptor site. As a result of the generally upward motion in
the airflow, the position with the greatest PCR from the four road traffic
sources is located at a certain height which is commonly influenced by the
distance of this location from the traffic source and the background wind
field (about 15 m in this study). The potential contribution of a road to
one of the receptor sites is also investigated under different wind
directions. The established system and the results can be used to understand
the characteristics of urban wind environment and to help the air pollution
control planning in urban areas.</p>
  </abstract>
    </article-meta>
  </front>
<body>
      

<sec id="Ch1.S1" sec-type="intro">
  <label>1</label><title>Introduction</title>
      <p id="d1e210">In recent decades, with the continuous development of urban construction in
China, urban environmental problems have become increasingly serious and
attracted widespread attention. According to the 2019 China Ecological
Environment Status Bulletin, 180 of 337 cities at the prefecture level
exceeded ambient air quality standards. The complex building layouts and
differences in thermal structures within cities lead to extremely
complicated meteorological characteristics and pollutant transport in urban
areas (Aynsley, 1989; Fernando et al., 2010; Lei et al., 2012). Though
the transport of atmospheric pollution in urban areas is widely studied, tracking the sources of pollutants at the street level is still
lacking due to limitations in research methods.</p>
      <?pagebreak page2222?><p id="d1e213">Research on the street-level atmospheric environment is mainly divided
into three methods: field measurements (Macdonald et al.,
1997), laboratory simulation research (Mavroidis et al.,
2003), and model simulations (Hendricks et al., 2007; Kochanski et al.,
2015; Miao et al., 2014). Model simulation has become one of the main
methods for studying environmental problems at the street level due to the
easy control of simulation conditions and simple processing steps. Computational fluid dynamics (CFD) is a numerical simulation method to study fluid thermal-dynamic problems and is now widely used in studies
related to microscale problems within the urban canopy
(Gosman, 1999). The core of the CFD simulation method is to
solve the Navier–Stokes equations. Depending on the turbulence closure
scheme, CFD models can be divided into three types: direct numerical
simulation (DNS), Reynolds-averaged Navier–Stokes (RANS) equations (Liu et al.,
2018; Milliez and Carissimo, 2008; Zheng et al., 2015), and large-eddy
simulation (LES) (Kurppa et al., 2018; Li et al., 2008; Sada and Sato,
2002). The choice among the three methods depends on the costs and
objectives. One of the most important issues using CFD simulation for
environment problems at the street level is to obtain accurate initial and
boundary conditions (Ehrhard et al., 2000). To solve this
problem, the multi-scale coupling method is revealed as a good solution,
which uses meteorological information from mesoscale models as the
initial and boundary conditions to drive CFD (Nelson
et al., 2016). Tewari et al. (2010) proved that
CFD simulation was improved significantly when the results of the Weather
Research and Forecasting (WRF) model were used as the initial and boundary
conditions. With the WRF model, the community multiscale air quality (CMAQ)
model, and the CFD (RANS) approach, Kwak et al. (2015)
built an urban air quality modelling system, which presented a better
performance than the WRF-CMAQ model in simulating nitrogen dioxide
(<inline-formula><mml:math id="M1" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">NO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>) and ozone (<inline-formula><mml:math id="M2" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>) concentrations.</p>
      <p id="d1e238">Nevertheless, street-level air pollutant transport resulting from
nearby sources was still not fully investigated. The Flexible Particle
(FLEXPART) model (Stohl, 2003; Stohl et al.,
2005) is a Lagrangian particle dispersion model. The FLEXPART model can track the transport of
tracers via forward or backward simulation. Different from an Eulerian model,
the Lagrangian model is not restricted by the Courant–Friedrichs–Lewy
(CFL) condition (Stam, 1999), and thus, the integration process in
the Lagrangian model can be maintained with high spatial resolution with
acceptable computation efficiency. Initially, the FLEXPART model was driven
by global meteorological reanalysis data from the European Centre for
Medium-Range Weather Forecasts (ECMWF) or National Centers for Environmental
Prediction (NCEP). Fast and Easter (2006) developed a FLEXPART version
that used the WRF model output and was optimized with technical level and
output results. Today, the WRF-FLEXPART model has been widely used to
research the regional transport of air pollutants (Brioude et al., 2013;
De Foy et al., 2011; Gao et al., 2020; J. He et al.,
2017; He et al., 2020; Yu
et al., 2020). Cécé et al. (2016) first applied
the FLEXPART model at a small-scale resolution to analyse potential sources
of nitrogen oxide (<inline-formula><mml:math id="M3" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">NO</mml:mi><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>) in urban areas, with the WRF model results as
the driving field. Though FLEXPART has been extensively applied in medium-
and long-range transport cases (Heo et al., 2015; Liu et al., 2013;
Madala et al., 2015; Sandeepan et al., 2013), it has been rarely tested for
street-level transport and small-scale resolution grids.</p>
      <p id="d1e252">The objective of the present work is to investigate the flow field
characteristics and potential contribution of traffic sources to receptor
sites, under real building scenarios and meteorological conditions. To this
end, a multi-model simulation system for street-level circulation and
pollutant tracking (S-TRACK) was developed by integrating the WRF mesoscale,
the STAR-CCM+ street scale, and the FLEXPART particle dispersion models
and applying them to the Jinshui District of Zhengzhou City, Henan Province.
Zhengzhou is located in central China with four distinct seasons.
According to the Oceanic Niño Index (ONI), an El Niño event occurred
in January 2019. The occurrence of El Niño generally favours a warm
winter and weak winter winds in China that are conducive to the occurrence of air
pollution. Therefore, the period of January 2019 was selected and simulated
for this study. This paper is organized as follows. Section 2 presents
the model details and the observed data for the model validation. Section 3
provides the details of the model validation results, the wind environment
characteristics, and the potential contribution of traffic sources to receptor
sites in the region. Section 4 provides the conclusions of the study.</p>
</sec>
<sec id="Ch1.S2">
  <label>2</label><title>Data and methods</title>
<sec id="Ch1.S2.SS1">
  <label>2.1</label><title>S-TRACK description</title>
      <p id="d1e270">The S-TRACK system consists of three major components (Fig. 1). The WRF
model is used to obtain the mesoscale three-dimensional (3D) meteorological
fields, with the initial and boundary conditions provided by NCEP FNL
reanalysis data. STAR-CCM+, driven by the meteorological data from
WRF, is used to compute the refined 3D street-level meteorological fields
with a resolution of 1 to 100 m in the simulation area. With the refined
3D meteorology, the FLEXPART model is run to analyse the transport of
traffic sources at street level and their potential contribution to specific
sites. One should note that some meteorological variables needed by FLEXPART
that STAR-CCM+ cannot provide (Table 1) are obtained from WRF
simulations. The specific coupling scheme of the S-TRACK system is detailed
as follows.
<list list-type="custom"><list-item><label>I.</label>
      <p id="d1e275"><italic>Run the WRF model</italic> (refer to Sect. 2.2 for specific settings)
to obtain meteorological data with a spatial resolution of <inline-formula><mml:math id="M4" display="inline"><mml:mrow><mml:mn mathvariant="normal">1</mml:mn><mml:mspace linebreak="nobreak" width="0.125em"/><mml:mrow class="unit"><mml:mi mathvariant="normal">km</mml:mi></mml:mrow><mml:mo>×</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:math></inline-formula> km, including temperature, pressure, humidity, wind, etc.</p></list-item><list-item><label>II.</label>
      <?pagebreak page2223?><p id="d1e297"><italic>Extract the value of temperature (</italic><inline-formula><mml:math id="M5" display="inline"><mml:mi>T</mml:mi></mml:math></inline-formula><italic>) and wind (</italic><inline-formula><mml:math id="M6" display="inline"><mml:mi>U</mml:mi></mml:math></inline-formula><italic>, </italic><inline-formula><mml:math id="M7" display="inline"><mml:mi>V</mml:mi></mml:math></inline-formula>,<italic> and </italic><inline-formula><mml:math id="M8" display="inline"><mml:mi>W</mml:mi></mml:math></inline-formula><italic>)</italic> from
the WRF simulation, as the initial and boundary conditions of the
STAR-CCM+ simulation. Run STAR-CCM+ (refer to Sect. 2.3 for
specific settings) to obtain values of meteorological variables with a
spatial resolution of 1–100 m, including wind field, surface pressure,
and surface sensible heat flux. The 3D street-level grid for
STAR-CCM+ is detailed in Sect. 2.3.1.</p></list-item><list-item><label>III.</label>
      <p id="d1e336"><italic>Match the STAR-CCM+ grids to the WRF grids.</italic> As the
FLEXPART-WRF (version 3.3.2) was used here, the grid structure of
meteorological input data to FLEXPART should match the grid structure of the WRF
model. To this end, a regular fine grid with a horizontal resolution of
<inline-formula><mml:math id="M9" display="inline"><mml:mrow><mml:mn mathvariant="normal">10</mml:mn><mml:mspace width="0.125em" linebreak="nobreak"/><mml:mrow class="unit"><mml:mi mathvariant="normal">m</mml:mi></mml:mrow><mml:mo>×</mml:mo><mml:mn mathvariant="normal">10</mml:mn></mml:mrow></mml:math></inline-formula> m was constructed based on the pre-processing system of the WRF
model (WPS). The urban building height data obtained based on drone aerial
photography were taken as part of the terrain height data in the WPS. Once
the refined grid was established, the meteorological variables of the
STAR-CCM+ and WRF models were interpolated into the grid by a
nearest-neighbour interpolation method.</p></list-item><list-item><label>IV.</label>
      <p id="d1e358"><italic>Run the backward FLEXPART model</italic> (refer to Sect. 2.4
for specific settings) to obtain the 3D spatial location data of released
particles, which were used to analyse the features of pollutant transport at
street level and the potential contribution of traffic sources to specific sites.</p></list-item></list></p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F1" specific-use="star"><?xmltex \currentcnt{1}?><?xmltex \def\figurename{Figure}?><label>Figure 1</label><caption><p id="d1e365">The S-TRACK system: the role of WRF, STAR-CCM+, and FLEXPART in
the S-TRACK system and the process of gradual refinement of resolution.</p></caption>
          <?xmltex \igopts{width=426.791339pt}?><graphic xlink:href="https://acp.copernicus.org/articles/22/2221/2022/acp-22-2221-2022-f01.png"/>

        </fig>

<?xmltex \floatpos{t}?><table-wrap id="Ch1.T1" specific-use="star"><?xmltex \currentcnt{1}?><label>Table 1</label><caption><p id="d1e377">The list of variables required to run FLEXPART and the
sources of variables.</p></caption><oasis:table frame="topbot"><oasis:tgroup cols="3">
     <oasis:colspec colnum="1" colname="col1" align="justify" colwidth="70pt"/>
     <oasis:colspec colnum="2" colname="col2" align="justify" colwidth="155pt"/>
     <oasis:colspec colnum="3" colname="col3" align="justify" colwidth="55pt"/>
     <oasis:thead>
       <oasis:row rowsep="1">
         <oasis:entry colname="col1">Variable</oasis:entry>
         <oasis:entry colname="col2">Description</oasis:entry>
         <oasis:entry colname="col3">Source</oasis:entry>
       </oasis:row>
     </oasis:thead>
     <oasis:tbody>
       <oasis:row>
         <oasis:entry colname="col1">PB</oasis:entry>
         <oasis:entry colname="col2">base value of pressure</oasis:entry>
         <oasis:entry colname="col3">WRF</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1"><inline-formula><mml:math id="M10" display="inline"><mml:mi>P</mml:mi></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col2">perturbation of pressure</oasis:entry>
         <oasis:entry colname="col3">WRF</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">PHB</oasis:entry>
         <oasis:entry colname="col2">base value of geopotential</oasis:entry>
         <oasis:entry colname="col3">WRF</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">PH</oasis:entry>
         <oasis:entry colname="col2">perturbation of geopotential</oasis:entry>
         <oasis:entry colname="col3">WRF</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1"><inline-formula><mml:math id="M11" display="inline"><mml:mi>T</mml:mi></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col2">temperature</oasis:entry>
         <oasis:entry colname="col3">WRF</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">QVAPOR</oasis:entry>
         <oasis:entry colname="col2">specific humidity</oasis:entry>
         <oasis:entry colname="col3">WRF</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">MAPFAC_M</oasis:entry>
         <oasis:entry colname="col2">map factor</oasis:entry>
         <oasis:entry colname="col3">WRF</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">PSFC</oasis:entry>
         <oasis:entry colname="col2">surface pressure</oasis:entry>
         <oasis:entry colname="col3">STAR-CCM+</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">U10</oasis:entry>
         <oasis:entry colname="col2">10 m wind along <inline-formula><mml:math id="M12" display="inline"><mml:mi>x</mml:mi></mml:math></inline-formula> axis</oasis:entry>
         <oasis:entry colname="col3">STAR-CCM+</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">V10</oasis:entry>
         <oasis:entry colname="col2">10 m wind along <inline-formula><mml:math id="M13" display="inline"><mml:mi>y</mml:mi></mml:math></inline-formula> axis</oasis:entry>
         <oasis:entry colname="col3">STAR-CCM+</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">T2</oasis:entry>
         <oasis:entry colname="col2">2 m temperature</oasis:entry>
         <oasis:entry colname="col3">WRF</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">Q2</oasis:entry>
         <oasis:entry colname="col2">2 m dew point</oasis:entry>
         <oasis:entry colname="col3">WRF</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">SWDOWN</oasis:entry>
         <oasis:entry colname="col2">surface solar radiation (optional)</oasis:entry>
         <oasis:entry colname="col3">WRF</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">RAINNC</oasis:entry>
         <oasis:entry colname="col2">large-scale precipitation (optional)</oasis:entry>
         <oasis:entry colname="col3">WRF</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">RAINC</oasis:entry>
         <oasis:entry colname="col2">convective precipitation (optional)</oasis:entry>
         <oasis:entry colname="col3">WRF</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">HFX</oasis:entry>
         <oasis:entry colname="col2">surface sensible heat flux (optional)</oasis:entry>
         <oasis:entry colname="col3">STAR-CCM+</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1"><inline-formula><mml:math id="M14" display="inline"><mml:mi>U</mml:mi></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col2">wind along <inline-formula><mml:math id="M15" display="inline"><mml:mi>x</mml:mi></mml:math></inline-formula> axis</oasis:entry>
         <oasis:entry colname="col3">STAR-CCM+</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1"><inline-formula><mml:math id="M16" display="inline"><mml:mi>V</mml:mi></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col2">wind along <inline-formula><mml:math id="M17" display="inline"><mml:mi>y</mml:mi></mml:math></inline-formula> axis</oasis:entry>
         <oasis:entry colname="col3">STAR-CCM+</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1"><inline-formula><mml:math id="M18" display="inline"><mml:mi>W</mml:mi></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col2">Cartesian vertical velocity</oasis:entry>
         <oasis:entry colname="col3">STAR-CCM+</oasis:entry>
       </oasis:row>
     </oasis:tbody>
   </oasis:tgroup></oasis:table></table-wrap>

</sec>
<sec id="Ch1.S2.SS2">
  <label>2.2</label><title>WRF model configuration</title>
      <p id="d1e701">In this study, the WRF model is configured with four nested domains (Fig. 2a), with the resolution of <inline-formula><mml:math id="M19" display="inline"><mml:mrow><mml:mn mathvariant="normal">27</mml:mn><mml:mspace width="0.125em" linebreak="nobreak"/><mml:mrow class="unit"><mml:mi mathvariant="normal">km</mml:mi></mml:mrow><mml:mo>×</mml:mo><mml:mn mathvariant="normal">27</mml:mn></mml:mrow></mml:math></inline-formula> km (<inline-formula><mml:math id="M20" display="inline"><mml:mrow><mml:mn mathvariant="normal">85</mml:mn><mml:mo>×</mml:mo><mml:mn mathvariant="normal">85</mml:mn></mml:mrow></mml:math></inline-formula> grid
cells), <inline-formula><mml:math id="M21" display="inline"><mml:mrow><mml:mn mathvariant="normal">9</mml:mn><mml:mspace linebreak="nobreak" width="0.125em"/><mml:mrow class="unit"><mml:mi mathvariant="normal">km</mml:mi></mml:mrow><mml:mo>×</mml:mo><mml:mn mathvariant="normal">9</mml:mn></mml:mrow></mml:math></inline-formula> km (<inline-formula><mml:math id="M22" display="inline"><mml:mrow><mml:mn mathvariant="normal">82</mml:mn><mml:mo>×</mml:mo><mml:mn mathvariant="normal">82</mml:mn></mml:mrow></mml:math></inline-formula> grid cells), <inline-formula><mml:math id="M23" display="inline"><mml:mrow><mml:mn mathvariant="normal">3</mml:mn><mml:mspace linebreak="nobreak" width="0.125em"/><mml:mrow class="unit"><mml:mi mathvariant="normal">km</mml:mi></mml:mrow><mml:mo>×</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:math></inline-formula> km (<inline-formula><mml:math id="M24" display="inline"><mml:mrow><mml:mn mathvariant="normal">82</mml:mn><mml:mo>×</mml:mo><mml:mn mathvariant="normal">82</mml:mn></mml:mrow></mml:math></inline-formula> grid cells), and <inline-formula><mml:math id="M25" display="inline"><mml:mrow><mml:mn mathvariant="normal">1</mml:mn><mml:mspace width="0.125em" linebreak="nobreak"/><mml:mrow class="unit"><mml:mi mathvariant="normal">km</mml:mi></mml:mrow><mml:mo>×</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:math></inline-formula> km (<inline-formula><mml:math id="M26" display="inline"><mml:mrow><mml:mn mathvariant="normal">61</mml:mn><mml:mo>×</mml:mo><mml:mn mathvariant="normal">61</mml:mn></mml:mrow></mml:math></inline-formula> grid cells). Vertically, there are 45 full eta levels from
the surface to 100 hPa, with 11 levels below 2 km, the
meteorological fields of which are used to drive STAR-CCM+. The innermost
nested region is shown in Fig. 2b, where the area focused in this study is
marked with a black box. The initial and boundary conditions of the WRF model
are obtained from the NCEP re-analysis data
(<uri>https://rda.ucar.edu/datasets/ds083.2/</uri>, last access: 18 May 2021). The boundary conditions are
updated every 6 h. Table 2 lists the selected physical parameterization
schemes. The time from 12:00 Beijing time (BJT) on 30 December 2018 to
23:00 BJT on 31 January 2019 is chosen as the modelling period, with the
simulation results recorded every hour.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F2" specific-use="star"><?xmltex \currentcnt{2}?><?xmltex \def\figurename{Figure}?><label>Figure 2</label><caption><p id="d1e822">Domain configuration of the WRF model: <bold>(a)</bold> the range of the four
nested domains (d1–d4); <bold>(b)</bold> the innermost nested domain (d4), within which
the black box represents the STAR-CCM+ simulation domain (extracted from
© Google Maps 2021).</p></caption>
          <?xmltex \igopts{width=426.791339pt}?><graphic xlink:href="https://acp.copernicus.org/articles/22/2221/2022/acp-22-2221-2022-f02.png"/>

        </fig>

<?xmltex \floatpos{t}?><table-wrap id="Ch1.T2" specific-use="star"><?xmltex \currentcnt{2}?><label>Table 2</label><caption><p id="d1e840">Parameterization scheme for the physical processes set up in
the WRF model.</p></caption><oasis:table frame="topbot"><oasis:tgroup cols="3">
     <oasis:colspec colnum="1" colname="col1" align="left"/>
     <oasis:colspec colnum="2" colname="col2" align="left"/>
     <oasis:colspec colnum="3" colname="col3" align="left"/>
     <oasis:thead>
       <oasis:row rowsep="1">
         <oasis:entry colname="col1">Physical management</oasis:entry>
         <oasis:entry colname="col2">Parameterization</oasis:entry>
         <oasis:entry colname="col3">Reference</oasis:entry>
       </oasis:row>
     </oasis:thead>
     <oasis:tbody>
       <oasis:row>
         <oasis:entry colname="col1">Microphysics scheme</oasis:entry>
         <oasis:entry colname="col2">Lin</oasis:entry>
         <oasis:entry colname="col3">Lin et al. (1983)</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">Longwave radiation scheme</oasis:entry>
         <oasis:entry colname="col2">RRTMG</oasis:entry>
         <oasis:entry colname="col3">Iacono et al. (2008)</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">Shortwave radiation scheme</oasis:entry>
         <oasis:entry colname="col2">RRTMG</oasis:entry>
         <oasis:entry colname="col3">Iacono et al. (2008)</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">Land surface scheme</oasis:entry>
         <oasis:entry colname="col2">Noah</oasis:entry>
         <oasis:entry colname="col3">Chen and Dudhia (2001)</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">Planetary boundary layer scheme</oasis:entry>
         <oasis:entry colname="col2">MYNN3</oasis:entry>
         <oasis:entry colname="col3">Nakanishi and Niino (2006)</oasis:entry>
       </oasis:row>
     </oasis:tbody>
   </oasis:tgroup></oasis:table></table-wrap>

</sec>
<sec id="Ch1.S2.SS3">
  <label>2.3</label><title>STAR-CCM+ configuration</title>
      <p id="d1e940">STAR-CCM+, one of the most commonly used commercial CFD softwares, was
selected for the street-level simulation. Previous studies had found an
excellent correlation between STAR-CCM+ simulated and measured values in
simulating environmental and meteorological problems at street level (Borge et al., 2018; Santiago et al., 2020; Santiago et al., 2017). The model has
functions such as geometric modelling, model pre-processing, the calculation
execution, and post-processing of results. More details on STAR-CCM+ can
be found at <uri>https://www.plm.automation.siemens.com/global/zh/products/simcenter/STAR-CCM.html</uri> (last access: 25 June 2021).</p>
<sec id="Ch1.S2.SS3.SSS1">
  <label>2.3.1</label><title>3D street-level grid generation</title>
      <p id="d1e953">The establishment of a 3D geometric model is based on the actual terrain and
building height data for the simulated area obtained through drone
aerial photography technology. Basic data such as the geometric shape of
urban buildings, roof height, and vector data of the top of buildings with
high resolution, high timeliness, and accuracy are used to construct a
realistic 3D geometric model for driving the STAR-CCM+ simulation. In the
process of model construction, the same shape as the actual building was
maintained to reduce the influence of model errors on the calculation
results (Fig. 3a). The length, width, and height of the STAR-CCM+
calculation domain are 13, 11, and 2 km, respectively, among which
nearly two-thirds of the buildings are distributed in the range of 10–40 m,
with the average height of the buildings being 32 m. The highest building in
the area is 390 m, and the lowest building is 6 m.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F3" specific-use="star"><?xmltex \currentcnt{3}?><?xmltex \def\figurename{Figure}?><label>Figure 3</label><caption><p id="d1e958">The computational domain of STAR-CCM+ is shown in <bold>(a)</bold>. The
sub-domain A is used for detailed analysis of the wind environment, and the
Bank School City (BSC) monitoring site is marked with the red dot.
Sub-domain B is used to analyse the potential contribution of traffic sources
to receptor sites in the region, with magenta dots (S1 and S2) indicating
the receptor sites and orange lines indicating the main roads. The polyhedral
mesh is used to divide the STAR-CCM+ simulation area. The mesh details of
the vertical cross section and building surface are shown in <bold>(b)</bold>, and the 3D
meshes are shown in <bold>(c)</bold>.</p></caption>
            <?xmltex \igopts{width=398.338583pt}?><graphic xlink:href="https://acp.copernicus.org/articles/22/2221/2022/acp-22-2221-2022-f03.png"/>

          </fig>

      <p id="d1e976">The geometric model domain is divided by polyhedral meshes (Fig. 3c). The
polyhedral mesh has much fewer cells than the traditional tetrahedral mesh,
but with a similar accuracy of calculation. Under the same number of grid
cells, the numerical simulation results of polyhedral grid cells are more
consistent with experimental data than tetrahedral grid cells
(Zhang et al., 2020). The grid cells on the
ground and near the buildings are much denser (Fig. 3b) (the minimum
resolution is about 1 m), so that the influence of the building on the flow
patterns can be described more accurately. In the end, the number of unit
grid cells generated is 382 181, and the number of nodes is 1 990 224.</p>
</sec>
<sec id="Ch1.S2.SS3.SSS2">
  <label>2.3.2</label><title>Physical model and boundary conditions</title>
      <p id="d1e987">STAR-CCM+ solves the RANS equations with the realizable k-<inline-formula><mml:math id="M27" display="inline"><mml:mi mathvariant="italic">ε</mml:mi></mml:math></inline-formula>
turbulence closure scheme in this study (Lei et al., 2004; L. Li et al., 2006; S. Li et al., 2019). The ground and building surfaces are set to be
no-slip, and the distribution of fluid velocity and pressure near the ground
and the building surface is described by the blended wall function. For the
coupling of the WRF model to STAR-CCM+, the values of temperature and wind
from the WRF simulation are extracted to establish the initial and boundary
conditions for STAR-CCM+. Since the variables obtained by the WRF simulation
have a relatively coarse resolution of 1 km, the velocity components (<inline-formula><mml:math id="M28" display="inline"><mml:mi>U</mml:mi></mml:math></inline-formula>, <inline-formula><mml:math id="M29" display="inline"><mml:mi>V</mml:mi></mml:math></inline-formula>,
and <inline-formula><mml:math id="M30" display="inline"><mml:mi>W</mml:mi></mml:math></inline-formula>) and the temperature are interpolated to the<?pagebreak page2224?> boundary of the STAR-CCM+
domain using the spline interpolation method and the linear interpolation
method, respectively. For the turbulence intensity and turbulence viscosity
ratio, the lateral and upper boundaries are set as constants with values of
0.1 and 10, respectively.</p>
</sec>
</sec>
<sec id="Ch1.S2.SS4">
  <label>2.4</label><title>FLEXPART configuration</title>
      <p id="d1e1027">The simulation area is set to sub-domain B in Fig. 3, with a horizontal
grid resolution of <inline-formula><mml:math id="M31" display="inline"><mml:mrow><mml:mn mathvariant="normal">10</mml:mn><mml:mspace width="0.125em" linebreak="nobreak"/><mml:mrow class="unit"><mml:mi mathvariant="normal">m</mml:mi></mml:mrow><mml:mo>×</mml:mo><mml:mn mathvariant="normal">10</mml:mn></mml:mrow></mml:math></inline-formula> m. The simulation time is from 01:00 BJT 1 January 2019 to 23:00 BJT 30 January 2019. The time step of FLEXPART
is 1 s, and the output time interval is 120 s. Through backward trajectory
simulation, the impact of traffic source on the receptor sites in the region
can be effectively analysed. Due to the high number of<?pagebreak page2225?> grid cells in the
region and the fact that increasing the number of released particles leads
to consuming more computational resources, the particle residence time is
set as 2 h, five tracer particles are released per hour, and the total
number of particles released was 3590.</p>
</sec>
<sec id="Ch1.S2.SS5">
  <label>2.5</label><title>Meteorological observation data</title>
      <p id="d1e1055">Hourly near-surface meteorological observations from the Bank School City
monitoring site (hereinafter referred to as the BSC monitoring site), including
2 m temperature (<inline-formula><mml:math id="M32" display="inline"><mml:mi>T</mml:mi></mml:math></inline-formula>), 2 m relative humidity (RH), surface pressure (<inline-formula><mml:math id="M33" display="inline"><mml:mi>P</mml:mi></mml:math></inline-formula>), 10 m
wind direction (WD), and 10 m wind speed (WS) in January 2019, are used to
evaluate the WRF and STAR-CCM+ simulation results, with the statistical
indexes including Pearson's correlation coefficient (<inline-formula><mml:math id="M34" display="inline"><mml:mi>R</mml:mi></mml:math></inline-formula>), root mean square
error (RMSE), mean bias (MB), and mean error (ME). The location of the BSC
monitoring site (latitude: 34.802375, longitude: 113.675237) is shown in Fig. 3.</p><?xmltex \hack{\newpage}?>
</sec>
</sec>
<sec id="Ch1.S3">
  <label>3</label><title>Results and discussions</title>
<sec id="Ch1.S3.SS1">
  <label>3.1</label><title>Model evaluation</title>
      <p id="d1e1096">The performance of the WRF model to simulate meteorological elements is an
important basis for the STAR-CCM+ and FLEXPART simulations. The hourly
meteorological data for January 2019 obtained from the innermost nested
simulation of the WRF model are selected to compare with observation data to
verify the WRF model. Table 3 lists the statistical results of <inline-formula><mml:math id="M35" display="inline"><mml:mi>T</mml:mi></mml:math></inline-formula>, RH, <inline-formula><mml:math id="M36" display="inline"><mml:mi>P</mml:mi></mml:math></inline-formula>, and
WS. <inline-formula><mml:math id="M37" display="inline"><mml:mi>T</mml:mi></mml:math></inline-formula> and RH are slightly underestimated, with MB values of
<inline-formula><mml:math id="M38" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1.86</mml:mn></mml:mrow></mml:math></inline-formula> K
and <inline-formula><mml:math id="M39" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">5.95</mml:mn></mml:mrow></mml:math></inline-formula> %, respectively, and <inline-formula><mml:math id="M40" display="inline"><mml:mi>P</mml:mi></mml:math></inline-formula> and WS are overestimated by the WRF
model, with MB values of 3.66 hPa and 1.44 <inline-formula><mml:math id="M41" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">m</mml:mi><mml:mspace width="0.125em" linebreak="nobreak"/><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>, respectively. The
<inline-formula><mml:math id="M42" display="inline"><mml:mi>R</mml:mi></mml:math></inline-formula> values for <inline-formula><mml:math id="M43" display="inline"><mml:mi>T</mml:mi></mml:math></inline-formula>, RH, and <inline-formula><mml:math id="M44" display="inline"><mml:mi>P</mml:mi></mml:math></inline-formula> are 0.80, 0.70, and 0.98, respectively, passing the
99 % significance test (see Appendix A2) and indicating that the variation
characteristics of <inline-formula><mml:math id="M45" display="inline"><mml:mi>T</mml:mi></mml:math></inline-formula>, RH, and <inline-formula><mml:math id="M46" display="inline"><mml:mi>P</mml:mi></mml:math></inline-formula> are well reproduced by the WRF model. WS is
generally overestimated by the WRF model (He et al., 2014; Temimi et al.,
2020), which is also found in the present study with the RMSE of 1.97 <inline-formula><mml:math id="M47" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">m</mml:mi><mml:mspace width="0.125em" linebreak="nobreak"/><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>. The performance of the near-surface meteorology obtained by the
WRF simulation is equivalent<?pagebreak page2226?> to previous studies
(Carvalho et al., 2012; J. J. He et al., 2017).</p>

<?xmltex \floatpos{t}?><table-wrap id="Ch1.T3"><?xmltex \currentcnt{3}?><label>Table 3</label><caption><p id="d1e1221">Statistical performances of the hourly near-surface
meteorology simulated by the WRF model.</p></caption><oasis:table frame="topbot"><oasis:tgroup cols="5">
     <oasis:colspec colnum="1" colname="col1" align="left"/>
     <oasis:colspec colnum="2" colname="col2" align="right"/>
     <oasis:colspec colnum="3" colname="col3" align="right"/>
     <oasis:colspec colnum="4" colname="col4" align="right"/>
     <oasis:colspec colnum="5" colname="col5" align="right"/>
     <oasis:thead>
       <oasis:row rowsep="1">
         <oasis:entry colname="col1"/>
         <oasis:entry colname="col2"><inline-formula><mml:math id="M48" display="inline"><mml:mi>R</mml:mi></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col3">MB</oasis:entry>
         <oasis:entry colname="col4">ME</oasis:entry>
         <oasis:entry colname="col5">RMSE</oasis:entry>
       </oasis:row>
     </oasis:thead>
     <oasis:tbody>
       <oasis:row>
         <oasis:entry colname="col1"><inline-formula><mml:math id="M49" display="inline"><mml:mi>T</mml:mi></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col2">0.80</oasis:entry>
         <oasis:entry colname="col3"><inline-formula><mml:math id="M50" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1.86</mml:mn></mml:mrow></mml:math></inline-formula> (K)</oasis:entry>
         <oasis:entry colname="col4">2.33 (K)</oasis:entry>
         <oasis:entry colname="col5">2.82 (K)</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">RH</oasis:entry>
         <oasis:entry colname="col2">0.70</oasis:entry>
         <oasis:entry colname="col3"><inline-formula><mml:math id="M51" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">5.95</mml:mn></mml:mrow></mml:math></inline-formula> (%)</oasis:entry>
         <oasis:entry colname="col4">11.5 (%)</oasis:entry>
         <oasis:entry colname="col5">15.0 (%)</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1"><inline-formula><mml:math id="M52" display="inline"><mml:mi>P</mml:mi></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col2">0.98</oasis:entry>
         <oasis:entry colname="col3">3.66 (hPa)</oasis:entry>
         <oasis:entry colname="col4">3.66 (hPa)</oasis:entry>
         <oasis:entry colname="col5">3.77 (hPa)</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">WS</oasis:entry>
         <oasis:entry colname="col2">0.45</oasis:entry>
         <oasis:entry colname="col3">1.44 (<inline-formula><mml:math id="M53" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">m</mml:mi><mml:mspace linebreak="nobreak" width="0.125em"/><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>)</oasis:entry>
         <oasis:entry colname="col4">1.58 (<inline-formula><mml:math id="M54" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">m</mml:mi><mml:mspace width="0.125em" linebreak="nobreak"/><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>)</oasis:entry>
         <oasis:entry colname="col5">1.97 (<inline-formula><mml:math id="M55" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">m</mml:mi><mml:mspace linebreak="nobreak" width="0.125em"/><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>)</oasis:entry>
       </oasis:row>
     </oasis:tbody>
   </oasis:tgroup></oasis:table></table-wrap>

      <?pagebreak page2227?><p id="d1e1419">Since the time-varying boundary conditions in the calculation domain of
STAR-CCM+ are obtained from the WRF model, the simulation performance of the WRF
model has an important influence on the STAR-CCM+ simulation results. The
wind has an important influence on the transport of air pollutants in the
area (Zhang et al., 2015). Figure 4
shows the hourly wind
observations and simulations at the BSC monitoring site in January 2019.
Both WRF and STAR-CCM+ overestimate the wind speed to certain degrees
(Fig. 4a). The average of observed wind speed is 0.92 <inline-formula><mml:math id="M56" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">m</mml:mi><mml:mspace linebreak="nobreak" width="0.125em"/><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>, and the
average of simulated value by WRF and STAR-CCM+ is 2.37 and
2.00 <inline-formula><mml:math id="M57" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">m</mml:mi><mml:mspace linebreak="nobreak" width="0.125em"/><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>, respectively. The <inline-formula><mml:math id="M58" display="inline"><mml:mi>R</mml:mi></mml:math></inline-formula> values of WRF and STAR-CCM+ are 0.45
and 0.67, respectively, passing the 99 % significance test and
demonstrating the refined STAR-CCM+ wind simulations are superior to that
of the WRF. This might be due to the fact that the resolution of the WRF
simulation is not fine enough, and the underlying surface is processed in a
parameterized way that cannot accurately describe the urban surface
roughness. For STAR-CCM+, the geometric model is used for the
underlying surface, which could better reflect the urban surface conditions
compared to parametric methods. Figure 4b shows the comparison results of
the observed and simulated wind directions. It can be seen that the change
of the wind direction is captured by STAR-CCM+ well. The wind
direction is verified by hit rates (HRs) (Schlünzen and Sokhi, 2008),
which are a reliable overall measure for describing model performance (see
Appendix A4). With desired accuracy between <inline-formula><mml:math id="M59" display="inline"><mml:mrow><mml:mo>±</mml:mo><mml:mn mathvariant="normal">45</mml:mn></mml:mrow></mml:math></inline-formula><inline-formula><mml:math id="M60" display="inline"><mml:mrow class="unit"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:mrow></mml:math></inline-formula>, the HRs are
calculated at 63 % and 51 % for STAR-CCM+ and WRF, respectively,
indicating that variations in wind direction have been basically captured
with a better performance for STAR-CCM+ simulations.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F4" specific-use="star"><?xmltex \currentcnt{4}?><?xmltex \def\figurename{Figure}?><label>Figure 4</label><caption><p id="d1e1485">Evaluation of the wind simulation results at the BSC monitoring
site (see in Fig. 3a): the simulated (by the WRF (blue line) and STAR-CCM+
(red line) models) and the observed (grey line) hourly
near-surface wind speeds <bold>(a)</bold> and wind directions <bold>(b)</bold>.</p></caption>
          <?xmltex \igopts{width=341.433071pt}?><graphic xlink:href="https://acp.copernicus.org/articles/22/2221/2022/acp-22-2221-2022-f04.png"/>

        </fig>

</sec>
<sec id="Ch1.S3.SS2">
  <label>3.2</label><title>The characteristics of the street-level wind fields</title>
      <p id="d1e1508">In urban areas, the complex spatial structure and layout of buildings have a
great influence on the street-level wind field
(Liu et al., 2018; Park et al., 2015), which
is a crucial meteorological factor that controls the transport of air
pollutants. The street-level wind field characteristics were simulated by
the S-TRACK and discussed comprehensively in this paper for the overall
average in January as well as for different background wind directions,
i.e. north, south, west and east.</p>
<sec id="Ch1.S3.SS2.SSS1">
  <label>3.2.1</label><title>The average wind field characteristics</title>
      <p id="d1e1518">Figure 5a and b illustrate the distribution of the average wind streamlines in
January at the height of 5 and 40 m, respectively. At the height of 5 m,
the wind field structure is more complicated (Fig. 5a) than that at 40 m
(Fig. 5b). The wind speed is relatively more intense in the areas where the
buildings are sparse and smaller. In addition, the flow fields diverge or
converge due to the layout of buildings and streets, causing the wind
direction inside blocks to differ from the background wind direction greatly.
As the density of buildings gradually decreases with the increases in
height, this phenomenon diminishes, reflected by the relatively more
consistent wind fields at 40 m (Fig. 5b). The phenomenon was also found in a
previous study (Sui et al., 2016).</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F5" specific-use="star"><?xmltex \currentcnt{5}?><?xmltex \def\figurename{Figure}?><label>Figure 5</label><caption><p id="d1e1523">The simulated wind streamlines at the height of 5 <bold>(a)</bold> and 40 m
<bold>(b)</bold> averaged in January 2019 in the whole S-TRACK simulation domain; the
simulated wind streamlines and divergence <bold>(c)</bold> at the near surface averaged
in January 2019 in the sub-domain A (see in Fig. 3a). The BSC monitoring
site is marked with red dot.</p></caption>
            <?xmltex \igopts{width=469.470472pt}?><graphic xlink:href="https://acp.copernicus.org/articles/22/2221/2022/acp-22-2221-2022-f05.png"/>

          </fig>

      <p id="d1e1541">To clearly show the details of the wind field, sub-domain A (Fig. 3a) with
complex building structures is selected from the entire computational
domain. The near-surface winds disperse or converge horizontally and rise or
subside vertically with the building (Fig. 5c). During the climb or fall
with the building, downwash winds with high wind speeds occur (as shown in
the red dashed circles). Due to the complexity of the building layout, local
circulation is formed on the west side of the BSC monitoring site, making
the airflow around the building on the south side of the station accumulate
and form an obvious convergence area (Fig. 5c), which is not conducive to
the air circulation and pollution transport (as shown in the red box).</p>
</sec>
<sec id="Ch1.S3.SS2.SSS2">
  <label>3.2.2</label><title>The wind field characteristics under different background wind directions</title>
      <p id="d1e1552">Figure 6 shows the distributions of near-surface wind and its divergence
under four different background wind directions. In general, the overall
wind direction in the area is consistent with the background wind direction,
but the airflow near the surface is significantly affected by the building
layout, thus forming local circulations with divergence or convergence
zones. The wind speeds in the areas with dense buildings are significantly
smaller than those in open areas (Fig. 6a-1, b-1, c-1, and d-1), which
is attributed to the obvious frictional dragging effect of the dense
buildings. The overall wind direction in the area is generally the same as
the background wind direction, but the airflow is diverged or converged by
the influence of the building layout, resulting in a great difference in
wind direction inside the block from the background. When the background
wind direction is north or west (Fig. 6b and c), the overall wind speed in
the area is relatively large. This is mainly due to the temperate monsoon
climate in Zhengzhou, where northwest and west winds prevail in winter and
wind speeds are relatively high.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F6" specific-use="star"><?xmltex \currentcnt{6}?><?xmltex \def\figurename{Figure}?><label>Figure 6</label><caption><p id="d1e1557">The wind field streamlines and divergences under the background
wind directions of east <bold>(a)</bold>, south <bold>(b)</bold>, west <bold>(c)</bold>, and north <bold>(d)</bold>. The BSC
monitoring site is marked with a red dot.</p></caption>
            <?xmltex \igopts{width=483.69685pt}?><graphic xlink:href="https://acp.copernicus.org/articles/22/2221/2022/acp-22-2221-2022-f06.png"/>

          </fig>

      <p id="d1e1578">It is found that the windward side of the building is mostly a divergence
zone, and the leeward side is mainly a convergence zone, which is more
obvious for higher buildings. When the airflow meets the building, the
airflow on the windward side of the building is blocked and thus spreads
outward, forming a divergence zone. The airflow on the leeward side of
the building converges and generates a vortex with lower wind speed, forming
a convergence zone. For example, at the BSC monitoring site, when the background
wind direction is west, the wind speed on the windward side of the building
is higher and diffused outward by the building blockage (Fig. 6c-2),
resulting in a significant divergence zone (Fig. 6c-3). High-rise buildings
have a greater impact on the wind field and cause a strong degree of
convergence and divergence. It can be seen that the degree of divergence or
convergence around the high-rise building is more significant than those
around low buildings in the area (Fig. 6b-3, c-3, and d-3). In addition,
the ventilation is better when the dominant airflow is in the same direction
as building layout (Fig. 6c). In the process of urban construction, the
influence of prevailing wind direction on the layout of buildings should be
considered, which could effectively improve the efficiency of urban
ventilation.</p>
</sec>
</sec>
<sec id="Ch1.S3.SS3">
  <label>3.3</label><title>Potential contribution of traffic sources</title>
      <p id="d1e1590">In this section, the S-TRACK system is used to analyse the potential
contribution of main traffic roads (R1–R4) in sub-domain B (Fig. 3a) to
several receptor sites nearby with different heights and locations with a
number of schools and residential areas. The widths of roads R1–R4 are about
45, 33, 20, and 18 m, respectively. Since detailed information on
road traffic emissions was not available, the road traffic emissions were
assumed to be uniformly distributed and with identical intensity in this
study. During the backward-trajectory simulation, as long as the particles
passed within 5 m in height above the road, they are considered to be a potential
contribution from the road emissions to the receptor site. Additionally, the
potential contribution of traffic source under different background wind
directions was also explored. The residence-time analysis (RTA), which has
been previously used to identify the accounted for contribution of emission
sources to air quality of receptors (Ashbaugh<?pagebreak page2228?> et al., 1985; Hopke et
al., 2005; Poirot et al., 2001; Salvador et al., 2008; Yu, 2017), was
selected in this study to assess the potential contribution ratio (PCR) of
the traffic source for receptors. The RTA is expressed as
            <disp-formula id="Ch1.Ex1"><mml:math id="M61" display="block"><mml:mrow><mml:msub><mml:mi>R</mml:mi><mml:mrow><mml:mi>i</mml:mi><mml:mo>,</mml:mo><mml:mi>j</mml:mi></mml:mrow></mml:msub><mml:mo>=</mml:mo><mml:mstyle displaystyle="true"><mml:mfrac style="display"><mml:mrow><mml:msub><mml:mi mathvariant="italic">τ</mml:mi><mml:mrow><mml:mi>i</mml:mi><mml:mo>,</mml:mo><mml:mi>j</mml:mi></mml:mrow></mml:msub></mml:mrow><mml:mi>t</mml:mi></mml:mfrac></mml:mstyle><mml:mo>,</mml:mo></mml:mrow></mml:math></disp-formula>
          where <inline-formula><mml:math id="M62" display="inline"><mml:mrow><mml:msub><mml:mi>R</mml:mi><mml:mrow><mml:mi>i</mml:mi><mml:mo>,</mml:mo><mml:mi>j</mml:mi></mml:mrow></mml:msub></mml:mrow></mml:math></inline-formula> indicates the contribution ratio of the grid <inline-formula><mml:math id="M63" display="inline"><mml:mrow><mml:mo>(</mml:mo><mml:mi>i</mml:mi><mml:mo>,</mml:mo><mml:mi>j</mml:mi><mml:mo>)</mml:mo></mml:mrow></mml:math></inline-formula> to
receptor, <inline-formula><mml:math id="M64" display="inline"><mml:mrow><mml:msub><mml:mi mathvariant="italic">τ</mml:mi><mml:mrow><mml:mi>i</mml:mi><mml:mo>,</mml:mo><mml:mi>j</mml:mi></mml:mrow></mml:msub></mml:mrow></mml:math></inline-formula> means the residence time in the grid <inline-formula><mml:math id="M65" display="inline"><mml:mrow><mml:mo>(</mml:mo><mml:mi>i</mml:mi><mml:mo>,</mml:mo><mml:mi>j</mml:mi><mml:mo>)</mml:mo></mml:mrow></mml:math></inline-formula>, and <inline-formula><mml:math id="M66" display="inline"><mml:mi>t</mml:mi></mml:math></inline-formula>
means the total residence time in all grid cells.</p>
<sec id="Ch1.S3.SS3.SSS1">
  <label>3.3.1</label><title>Potential contribution of traffic sources at different sites in winter</title>
      <p id="d1e1707">In order to analyse the potential contribution of the traffic source to
different locations, the receptor sites were selected at different locations
and heights, and the overall PCR of all wind directions for January 2019 was
calculated by RTA (Table 4). Receptor sites S2–S8, with an identical horizontal
location but different heights, are selected to investigate<?pagebreak page2229?> contributions of
traffic sources to receptor sites at different heights. The PCR of all
four roads are 4.05 %, 4.25 %, 4.33 %, and 4.67 % for receptor sites
S2 to S5, with heights of 2, 5, 10, and 15 m, respectively.
However, as the receptor height continues to rise, namely from S5 to S8, the
PCR of the roads gradually decreases from 4.67 % to 3.55 % (Table 4).
It is noteworthy that the contributions from R1 and R3 are primary,
especially R1, which may be due to the closer distance to the site and
the generally northeast wind field. The potential contribution of the
traffic source is the greatest when the receptor site is located at a height
of 15 m, suggesting the air quality at that height is most susceptible to
traffic emissions under the northeast wind field. In addition, according to
density distribution (refers to the number of particles that have stayed in
the space of <inline-formula><mml:math id="M67" display="inline"><mml:mrow><mml:mn mathvariant="normal">10</mml:mn><mml:mspace width="0.125em" linebreak="nobreak"/><mml:mrow class="unit"><mml:mi mathvariant="normal">m</mml:mi></mml:mrow><mml:mo>×</mml:mo><mml:mn mathvariant="normal">10</mml:mn></mml:mrow></mml:math></inline-formula> m in the horizontal direction and 5 m from
the surface to above in the vertical direction) of all trajectory points
that have passed through the traffic roads (Fig. 7), it can be seen that
the road section with a large potential contribution to the receptor sites is
generally located to their northeast, which might be a result of the
combination effect of the background wind field and the building layout. For
more details, the vertical structure of winds along the direction of the
wind field at the receptor site S2 (Fig. 8b) is also presented. It can be
seen that there is a general upward motion in the airflow, showing the
position with the greatest PCR from traffic sources is located at a certain
height, which is about 15 m over the receptor site S2 in this case.</p>

<?xmltex \floatpos{t}?><table-wrap id="Ch1.T4" specific-use="star"><?xmltex \currentcnt{4}?><label>Table 4</label><caption><p id="d1e1729">Locations of receptor sites and the corresponding PCR.</p></caption><oasis:table frame="topbot"><oasis:tgroup cols="7">
     <oasis:colspec colnum="1" colname="col1" align="left"/>
     <oasis:colspec colnum="2" colname="col2" align="center"/>
     <oasis:colspec colnum="3" colname="col3" align="right"/>
     <oasis:colspec colnum="4" colname="col4" align="right"/>
     <oasis:colspec colnum="5" colname="col5" align="right"/>
     <oasis:colspec colnum="6" colname="col6" align="right"/>
     <oasis:colspec colnum="7" colname="col7" align="right"/>
     <oasis:thead>
       <oasis:row>
         <oasis:entry colname="col1">Receptor site</oasis:entry>
         <oasis:entry colname="col2">Location <inline-formula><mml:math id="M68" display="inline"><mml:mrow><mml:mo>(</mml:mo><mml:mi>x</mml:mi><mml:mo>,</mml:mo><mml:mi>y</mml:mi><mml:mo>,</mml:mo><mml:mi>z</mml:mi><mml:mo>)</mml:mo></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry rowsep="1" namest="col3" nameend="col7" align="center">PCR </oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">
         <oasis:entry colname="col1"/>
         <oasis:entry colname="col2"/>
         <oasis:entry colname="col3">R1</oasis:entry>
         <oasis:entry colname="col4">R2</oasis:entry>
         <oasis:entry colname="col5">R3</oasis:entry>
         <oasis:entry colname="col6">R4</oasis:entry>
         <oasis:entry colname="col7">All</oasis:entry>
       </oasis:row>
     </oasis:thead>
     <oasis:tbody>
       <oasis:row>
         <oasis:entry colname="col1">S1</oasis:entry>
         <oasis:entry colname="col2">(<inline-formula><mml:math id="M69" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">3200</mml:mn></mml:mrow></mml:math></inline-formula> m, <inline-formula><mml:math id="M70" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1420</mml:mn></mml:mrow></mml:math></inline-formula> m, 2 m)</oasis:entry>
         <oasis:entry colname="col3">1.81 %</oasis:entry>
         <oasis:entry colname="col4">–</oasis:entry>
         <oasis:entry colname="col5">–</oasis:entry>
         <oasis:entry colname="col6">–</oasis:entry>
         <oasis:entry colname="col7">–</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">S2</oasis:entry>
         <oasis:entry colname="col2">(<inline-formula><mml:math id="M71" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">2500</mml:mn></mml:mrow></mml:math></inline-formula> m, <inline-formula><mml:math id="M72" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1300</mml:mn></mml:mrow></mml:math></inline-formula> m, 2 m)</oasis:entry>
         <oasis:entry colname="col3">2.38 %</oasis:entry>
         <oasis:entry colname="col4">0.18 %</oasis:entry>
         <oasis:entry colname="col5"><italic>1.32 %</italic></oasis:entry>
         <oasis:entry colname="col6">0.16 %</oasis:entry>
         <oasis:entry colname="col7">4.05 %</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">S3</oasis:entry>
         <oasis:entry colname="col2">(<inline-formula><mml:math id="M73" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">2500</mml:mn></mml:mrow></mml:math></inline-formula> m, <inline-formula><mml:math id="M74" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1300</mml:mn></mml:mrow></mml:math></inline-formula> m, 5 m)</oasis:entry>
         <oasis:entry colname="col3">2.57 %</oasis:entry>
         <oasis:entry colname="col4">0.29 %</oasis:entry>
         <oasis:entry colname="col5">1.28 %</oasis:entry>
         <oasis:entry colname="col6">0.10 %</oasis:entry>
         <oasis:entry colname="col7">4.25 %</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">S4</oasis:entry>
         <oasis:entry colname="col2">(<inline-formula><mml:math id="M75" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">2500</mml:mn></mml:mrow></mml:math></inline-formula> m, <inline-formula><mml:math id="M76" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1300</mml:mn></mml:mrow></mml:math></inline-formula> m, 10 m)</oasis:entry>
         <oasis:entry colname="col3">2.71 %</oasis:entry>
         <oasis:entry colname="col4">0.32 %</oasis:entry>
         <oasis:entry colname="col5">1.18 %</oasis:entry>
         <oasis:entry colname="col6">0.12 %</oasis:entry>
         <oasis:entry colname="col7">4.33 %</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">S5</oasis:entry>
         <oasis:entry colname="col2">(<inline-formula><mml:math id="M77" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">2500</mml:mn></mml:mrow></mml:math></inline-formula> m, <inline-formula><mml:math id="M78" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1300</mml:mn></mml:mrow></mml:math></inline-formula> m, 15 m)</oasis:entry>
         <oasis:entry colname="col3"><italic>2.98 %</italic></oasis:entry>
         <oasis:entry colname="col4">0.27 %</oasis:entry>
         <oasis:entry colname="col5">1.22 %</oasis:entry>
         <oasis:entry colname="col6">0.20 %</oasis:entry>
         <oasis:entry colname="col7"><italic>4.67 %</italic></oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">S6</oasis:entry>
         <oasis:entry colname="col2">(<inline-formula><mml:math id="M79" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">2500</mml:mn></mml:mrow></mml:math></inline-formula> m, <inline-formula><mml:math id="M80" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1300</mml:mn></mml:mrow></mml:math></inline-formula> m, 20 m)</oasis:entry>
         <oasis:entry colname="col3">2.75 %</oasis:entry>
         <oasis:entry colname="col4">0.37 %</oasis:entry>
         <oasis:entry colname="col5">1.09 %</oasis:entry>
         <oasis:entry colname="col6">0.17 %</oasis:entry>
         <oasis:entry colname="col7">4.38 %</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">S7</oasis:entry>
         <oasis:entry colname="col2">(<inline-formula><mml:math id="M81" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">2500</mml:mn></mml:mrow></mml:math></inline-formula> m, <inline-formula><mml:math id="M82" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1300</mml:mn></mml:mrow></mml:math></inline-formula> m, 40 m)</oasis:entry>
         <oasis:entry colname="col3">2.30 %</oasis:entry>
         <oasis:entry colname="col4">0.39 %</oasis:entry>
         <oasis:entry colname="col5">0.70 %</oasis:entry>
         <oasis:entry colname="col6">0.25 %</oasis:entry>
         <oasis:entry colname="col7">3.64 %</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">S8</oasis:entry>
         <oasis:entry colname="col2">(<inline-formula><mml:math id="M83" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">2500</mml:mn></mml:mrow></mml:math></inline-formula> m, <inline-formula><mml:math id="M84" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1300</mml:mn></mml:mrow></mml:math></inline-formula> m, 50 m)</oasis:entry>
         <oasis:entry colname="col3">1.94 %</oasis:entry>
         <oasis:entry colname="col4">0.57 %</oasis:entry>
         <oasis:entry colname="col5">0.68 %</oasis:entry>
         <oasis:entry colname="col6">0.36 %</oasis:entry>
         <oasis:entry colname="col7">3.55 %</oasis:entry>
       </oasis:row>
     </oasis:tbody>
   </oasis:tgroup></oasis:table></table-wrap>

      <?xmltex \floatpos{t}?><fig id="Ch1.F7" specific-use="star"><?xmltex \currentcnt{7}?><?xmltex \def\figurename{Figure}?><label>Figure 7</label><caption><p id="d1e2178">Density distribution on the road of backward trajectory particles released from different receptor sites (S1, S2, S5, and
S7; see details in Table 4). The four receptor sites are all marked with
magenta dots.</p></caption>
            <?xmltex \igopts{width=483.69685pt}?><graphic xlink:href="https://acp.copernicus.org/articles/22/2221/2022/acp-22-2221-2022-f07.png"/>

          </fig>

      <?xmltex \floatpos{t}?><fig id="Ch1.F8" specific-use="star"><?xmltex \currentcnt{8}?><?xmltex \def\figurename{Figure}?><label>Figure 8</label><caption><p id="d1e2190">The <bold>(a)</bold> average surface wind and <bold>(b)</bold> vertical structure of average
winds along the wind direction around the receptor site S2 (line AB) in
January 2019. The road R1 is marked with an orange line, the location of the
vertical profile is shown as a black line, and the receptor sites S1 to S6 are
all marked with magenta dots.</p></caption>
            <?xmltex \igopts{width=497.923228pt}?><graphic xlink:href="https://acp.copernicus.org/articles/22/2221/2022/acp-22-2221-2022-f08.png"/>

          </fig>

      <p id="d1e2205">It can be seen from Table 4 that R1 is the road with the greatest potential
contribution to the receptor sites. The horizontal distance between road R1
and the receptor sites is about 300 m, and the peak of the PCR occurs at a
height of about 15 m (corresponding to the site S5). However, for the road
R3, which is closest to the receptor sites in the horizontal (about 200 m), the
contribution ratios are lower than those of the road R1. Figure 8a shows
that the near-ground winds are generally northeast, resulting in the
probability of traffic contributions from R1 and R3 road sections upwind of
the site S2 being roughly the same. Nonetheless, as mentioned in Sect. 3.3,
the width for the road R1 is about twice that of the road R3. Therefore,
even though R1 was a little farther from the receptor sites than R3, the
contribution ratios of R1 to the sites were calculated to be larger than those of
R3. For R2 and R4, the distance from the receptor sites is about 1200
and 1500 m, respectively, farther away than those of R1 and<?pagebreak page2230?> R3. In addition,
under northeast winds, the traffic source was hardly transported to the
receptor sites, rendering the contribution ratios quite small below 50 m
(Table 4). It can also be seen, from Table 4, that the corresponding PCR of
R2 and R4 may peak at a height over 50 m.</p>
      <p id="d1e2208">Since the road R1 had the largest potential contribution to the receptor
sites, the contribution of R1 to different positions is focused in the
subsequent discussion. For the receptor site S1, which is about 400 m from R1, located in a dense building area with the building height at 30 to
40 m, the PCR of the traffic source to the receptor site is calculated
to be 1.81 %. For the receptor site S2, which is about 300 m from the
traffic road, located in an open area and surrounded by low buildings, the
PCR of the traffic source is determined to be 2.38 %. It might be inferred
that the wind field difference partially resulted from the influence of
building layout and led to the higher contribution ratio to S2. From the
average wind field in January 2019 (Fig. 8a), it can be seen that the winds
were influenced by high-rise buildings around S1, resulting in a change
in transport path of pollutants and thus making it difficult for pollutants to
reach the S1 site. However, for the S2 site, the winds were less influenced by
the buildings, and pollutants were more easily transported there.</p>
</sec>
<sec id="Ch1.S3.SS3.SSS2">
  <label>3.3.2</label><title>Potential contribution of traffic sources under different background
wind directions</title>
      <p id="d1e2219">In order to investigate the potential contribution of traffic sources under
different background wind directions, the receptor site S2 influenced by
R1 under the east, the south, the west, and the north wind directions was
classified from<?pagebreak page2231?> the simulation period. The PCRs of the traffic source were
estimated to be 2.45 %, 0.07 %, 1.98 %, and 2.97 % for the east, the
south, the west, and the north wind directions, respectively, revealing that
the difference in potential contribution was largest between the south and
north wind directions. When the background wind direction was south, the
receptor site was located upwind of the road, and the road traffic source
contributed very little to the receptor site. On the contrary, when the
receptor site was downwind of the road with northern winds, the contribution
ratio of road traffic source to the receptor site was the greatest. When the
background wind direction was east and west, the contribution ratio to the
receptor point was similar, ranging between the ratios under the south and north
wind directions. The lower contribution ratio during westerly winds
relative to that under easterly winds might partially be due to the denser
distribution of buildings upwind of the receptor site. Complex building
layouts changed the structure of the wind field and thus had an impact on
the transport of pollutants. The slow air circulation in dense building
areas made it unfavourable for pollutants to be transported. In the windward
side of the dense building area, the wind was blocked and diverted to both
sides of the building. Pollutants were difficult to transport to the leeward
side of the building, where the receptor site was located. The results of
the potential contribution of traffic sources under different background wind
conditions are helpful to understand the street-level pollution transport
characteristics and provide effective suggestions for the traffic pollution
control strategies.</p>
</sec>
</sec>
</sec>
<sec id="Ch1.S4" sec-type="conclusions">
  <label>4</label><title>Conclusions</title>
      <p id="d1e2232">A street-level pollutant tracking system has been developed to simulate
micro-scale meteorology and used to analyse the characteristics of wind
environment and the potential traffic source contribution of air pollution
to receptors through backward simulations in a city district. In general,
the S-TRACK system is effective in simulating street-level
meteorological and pollution problems. The presence of buildings has a
significant effect on the wind environment; i.e. the dragging effect of
dense buildings renders the wind speed inside the block smaller than the
background wind speed. The ventilation is better when the dominant airflow
is consistent with the direction of building layout. Influenced by the
building layout, the airflow near the surface is formed with divergence and
convergence zones. The windward side of the building is mostly a divergence
zone, and the leeward side is mostly a convergence zone, which is more
obvious for higher buildings.</p>
      <p id="d1e2235">As a test case, the S-TRACK system has been used to investigate the
potential contribution of traffic sources to receptor sites with different
locations, heights, and background wind directions in a city district. For a
specific location of this case study, the potential traffic contribution
ratios also varied with height at about 4.05 %, 4.25 %, 4.33 %,
4.67 %, 4.38 %, 3.64 %, and 3.55 % for 2, 5, 10, 15, 20, 40, and 50 m,
respectively, manifesting a significant trend of increasing and then
decreasing with height. In addition, the height of position with the
greatest PCR from the traffic source varies jointly, influenced by the
distance between the position and traffic source, as well as the background
wind field. The potential contribution of traffic sources to a specific
receptor site varies under different background wind directions, which are
estimated to be 2.45 %, 0.07 %, 1.98 %, and 2.97 % for the east, the
south, the west, and the north wind directions, respectively. The difference
in potential contribution under east and west wind directions might
partially be due to the density of buildings upwind of the receptor site.</p>
      <p id="d1e2238">In the future, in-depth simulation experiments with different building
layouts, wind field environments, and<?pagebreak page2232?> distances between traffic source and
receptor are required to quantify the potential contribution of street-level
pollution sources and to establish the relationship between meteorological
conditions, buildings, and various emissions (point, area, and line sources)
in the street level for an effective management of regional pollution in a
city.</p>
</sec>

      
      </body>
    <back><app-group>

<app id="App1.Ch1.S1">
  <?xmltex \currentcnt{A}?><label>Appendix A</label><title/>
<sec id="App1.Ch1.S1.SS1">
  <label>A1</label><title>Some settings to improve the calculation efficiency of CFD</title>
      <p id="d1e2259">It is true that using a CFD model for the atmospheric numerical simulation
has the problem of high computational cost. In this study, RANS equations are
chosen as the CFD model, which requires a relatively small amount of
computational resources. The time step of STAR-CCM+ is set to 60 s, with a
maximum of 20 internal iterations in each time step, and a parallel computing
with 32 CPUs is done on a supercomputer. The simulation error increases with
the simulation time. In order to ensure the efficiency and accuracy of the
simulation, the month was divided into four time periods to simulate, as
shown in Table A1.</p>

<?xmltex \floatpos{h!}?><table-wrap id="App1.Ch1.S1.T5"><?xmltex \hack{\hsize\textwidth}?><?xmltex \currentcnt{A1}?><label>Table A1</label><caption><p id="d1e2266">The division of each simulation time period and the
physical time spent on the simulation.</p></caption><oasis:table frame="topbot"><oasis:tgroup cols="4">
     <oasis:colspec colnum="1" colname="col1" align="left"/>
     <oasis:colspec colnum="2" colname="col2" align="right"/>
     <oasis:colspec colnum="3" colname="col3" align="right"/>
     <oasis:colspec colnum="4" colname="col4" align="right"/>
     <oasis:thead>
       <oasis:row rowsep="1">
         <oasis:entry colname="col1">Simulation start time</oasis:entry>
         <oasis:entry colname="col2">Simulation end time</oasis:entry>
         <oasis:entry colname="col3">Length of simulation time</oasis:entry>
         <oasis:entry colname="col4">Physical time spent</oasis:entry>
       </oasis:row>
     </oasis:thead>
     <oasis:tbody>
       <oasis:row>
         <oasis:entry colname="col1">2018/12/31 00:00:00</oasis:entry>
         <oasis:entry colname="col2">2019/01/09 04:00:00</oasis:entry>
         <oasis:entry colname="col3">220 h</oasis:entry>
         <oasis:entry colname="col4">126.45 h</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">2019/01/08 00:00:00</oasis:entry>
         <oasis:entry colname="col2">2019/01/17 04:00:00</oasis:entry>
         <oasis:entry colname="col3">220 h</oasis:entry>
         <oasis:entry colname="col4">128.33 h</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">2019/01/16 00:00:00</oasis:entry>
         <oasis:entry colname="col2">2019/01/25 04:00:00</oasis:entry>
         <oasis:entry colname="col3">220 h</oasis:entry>
         <oasis:entry colname="col4">128.53 h</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">2019/01/24 00:00:00</oasis:entry>
         <oasis:entry colname="col2">2019/02/01 08:00:00</oasis:entry>
         <oasis:entry colname="col3">200 h</oasis:entry>
         <oasis:entry colname="col4">117.10 h</oasis:entry>
       </oasis:row>
     </oasis:tbody>
   </oasis:tgroup></oasis:table></table-wrap>

<?xmltex \floatpos{h!}?><table-wrap id="App1.Ch1.S1.T6"><?xmltex \currentcnt{A2}?><label>Table A2</label><caption><p id="d1e2367">The location of each meteorological station and the
average wind speed.</p></caption><oasis:table frame="topbot"><oasis:tgroup cols="3">
     <oasis:colspec colnum="1" colname="col1" align="left"/>
     <oasis:colspec colnum="2" colname="col2" align="center"/>
     <oasis:colspec colnum="3" colname="col3" align="right"/>
     <oasis:thead>
       <oasis:row>
         <oasis:entry colname="col1">Number</oasis:entry>
         <oasis:entry colname="col2">Latitude and longitude</oasis:entry>
         <oasis:entry colname="col3">Average wind</oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">
         <oasis:entry colname="col1"/>
         <oasis:entry colname="col2">coordinates</oasis:entry>
         <oasis:entry colname="col3">speed</oasis:entry>
       </oasis:row>
     </oasis:thead>
     <oasis:tbody>
       <oasis:row>
         <oasis:entry colname="col1">1</oasis:entry>
         <oasis:entry colname="col2">(34.7274, 113.7493)</oasis:entry>
         <oasis:entry colname="col3">0.92 <inline-formula><mml:math id="M85" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">m</mml:mi><mml:mspace linebreak="nobreak" width="0.125em"/><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula></oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">2</oasis:entry>
         <oasis:entry colname="col2">(34.73506, 113.6457)</oasis:entry>
         <oasis:entry colname="col3">0.92 <inline-formula><mml:math id="M86" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">m</mml:mi><mml:mspace linebreak="nobreak" width="0.125em"/><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula></oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">3</oasis:entry>
         <oasis:entry colname="col2">(34.7466, 113.6876)</oasis:entry>
         <oasis:entry colname="col3">1.32 <inline-formula><mml:math id="M87" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">m</mml:mi><mml:mspace width="0.125em" linebreak="nobreak"/><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula></oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">4</oasis:entry>
         <oasis:entry colname="col2">(34.76117, 113.6883)</oasis:entry>
         <oasis:entry colname="col3">0.61 <inline-formula><mml:math id="M88" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">m</mml:mi><mml:mspace linebreak="nobreak" width="0.125em"/><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula></oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">5</oasis:entry>
         <oasis:entry colname="col2">(34.78245, 113.6567)</oasis:entry>
         <oasis:entry colname="col3">1.51 <inline-formula><mml:math id="M89" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">m</mml:mi><mml:mspace linebreak="nobreak" width="0.125em"/><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula></oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">6</oasis:entry>
         <oasis:entry colname="col2">(34.81151, 113.6948)</oasis:entry>
         <oasis:entry colname="col3">1.48 <inline-formula><mml:math id="M90" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">m</mml:mi><mml:mspace width="0.125em" linebreak="nobreak"/><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula></oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">7</oasis:entry>
         <oasis:entry colname="col2">(34.83267, 113.5453)</oasis:entry>
         <oasis:entry colname="col3">0.72 <inline-formula><mml:math id="M91" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">m</mml:mi><mml:mspace width="0.125em" linebreak="nobreak"/><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula></oasis:entry>
       </oasis:row>
     </oasis:tbody>
   </oasis:tgroup></oasis:table></table-wrap>

<?xmltex \hack{\newpage}?><?xmltex \floatpos{h!}?><fig id="App1.Ch1.S1.F9"><?xmltex \currentcnt{A1}?><?xmltex \def\figurename{Figure}?><label>Figure A1</label><caption><p id="d1e2611">Time series of the observed (black) and simulated (red)
PBLH at 08:00 and 20:00 Beijing time (BJT) at the Zhengzhou sounding site.</p></caption>
          <?xmltex \igopts{width=236.157874pt}?><graphic xlink:href="https://acp.copernicus.org/articles/22/2221/2022/acp-22-2221-2022-f09.png"/>

        </fig>

<?xmltex \hack{\clearpage}?>
</sec>
<?pagebreak page2233?><sec id="App1.Ch1.S1.SS2">
  <label>A2</label><title>Significance test</title>
      <p id="d1e2630">A significance test is used to determine the significance of the results in
relation to the null hypothesis, with a <inline-formula><mml:math id="M92" display="inline"><mml:mi>p</mml:mi></mml:math></inline-formula> value, or probability value,
describing how likely the data would have occurred by random chance (i.e.
that the null hypothesis is true). A <inline-formula><mml:math id="M93" display="inline"><mml:mi>p</mml:mi></mml:math></inline-formula> value less than 0.05 (typically <inline-formula><mml:math id="M94" display="inline"><mml:mrow><mml:mo>≤</mml:mo><mml:mn mathvariant="normal">0.05</mml:mn></mml:mrow></mml:math></inline-formula>) is statistically significant. It indicates strong evidence against
the null hypothesis, as there is less than a 5 % probability the null is
correct.</p>
</sec>
<sec id="App1.Ch1.S1.SS3">
  <label>A3</label><title>The observed data for January 2019 at various meteorological stations in
Zhengzhou city</title>
</sec>
<sec id="App1.Ch1.S1.SS4">
  <label>A4</label><title>Hit rates</title>
      <p id="d1e2673">The hit rate is a reliable overall measure for describing model performance.

                <disp-formula specific-use="align"><mml:math id="M95" display="block"><mml:mtable displaystyle="true"><mml:mtr><mml:mtd><mml:mstyle displaystyle="true" class="stylechange"/></mml:mtd><mml:mtd><mml:mrow><mml:mstyle class="stylechange" displaystyle="true"/><mml:mi>H</mml:mi><mml:mo>=</mml:mo><mml:mstyle displaystyle="true"><mml:mfrac style="display"><mml:mn mathvariant="normal">100</mml:mn><mml:mi>m</mml:mi></mml:mfrac></mml:mstyle><mml:mo>×</mml:mo><mml:munderover><mml:mo movablelimits="false">∑</mml:mo><mml:mrow><mml:mi>i</mml:mi><mml:mo>=</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow><mml:mi>m</mml:mi></mml:munderover><mml:msub><mml:mi>n</mml:mi><mml:mi>i</mml:mi></mml:msub></mml:mrow></mml:mtd></mml:mtr><mml:mtr><mml:mtd><mml:mstyle displaystyle="true" class="stylechange"/></mml:mtd><mml:mtd><mml:mrow><mml:mstyle class="stylechange" displaystyle="true"/><mml:mtext>with </mml:mtext><mml:msub><mml:mi>n</mml:mi><mml:mi>i</mml:mi></mml:msub><mml:mo>=</mml:mo><mml:mfenced open="{" close=""><mml:mtable columnspacing="1em" class="cases" rowspacing="0.2ex" columnalign="left left" framespacing="0em"><mml:mtr><mml:mtd><mml:mn mathvariant="normal">1</mml:mn></mml:mtd><mml:mtd><mml:mrow><mml:mtext>for </mml:mtext><mml:mi mathvariant="normal">|</mml:mi><mml:mtext> difference (measurement,</mml:mtext></mml:mrow></mml:mtd></mml:mtr><mml:mtr><mml:mtd><mml:mrow/></mml:mtd><mml:mtd><mml:mrow><mml:mspace linebreak="nobreak" width="1em"/><mml:mtext>model result)</mml:mtext><mml:mi mathvariant="normal">|</mml:mi><mml:mo>&lt;</mml:mo><mml:mi>A</mml:mi></mml:mrow></mml:mtd></mml:mtr><mml:mtr><mml:mtd><mml:mn mathvariant="normal">0</mml:mn></mml:mtd><mml:mtd><mml:mrow><mml:mtext>for </mml:mtext><mml:mi mathvariant="normal">|</mml:mi><mml:mtext> difference (measurement,</mml:mtext></mml:mrow></mml:mtd></mml:mtr><mml:mtr><mml:mtd><mml:mrow/></mml:mtd><mml:mtd><mml:mrow><mml:mspace linebreak="nobreak" width="1em"/><mml:mtext>model result)</mml:mtext><mml:mi mathvariant="normal">|</mml:mi><mml:mo>&gt;</mml:mo><mml:mi>A</mml:mi><mml:mo>,</mml:mo></mml:mrow></mml:mtd></mml:mtr></mml:mtable></mml:mfenced></mml:mrow></mml:mtd></mml:mtr></mml:mtable></mml:math></disp-formula>

            where <inline-formula><mml:math id="M96" display="inline"><mml:mi>m</mml:mi></mml:math></inline-formula> is the number of comparison data, and <inline-formula><mml:math id="M97" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula> is to consider the desired model
accuracy. The single hit rate is calculated ranging from 100 % if all
model results are within <inline-formula><mml:math id="M98" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula> of the observations to 0 % if none are.</p>
</sec>
<sec id="App1.Ch1.S1.SS5">
  <label>A5</label><title>Divergence</title>
      <p id="d1e2818">The divergence is a quantity that describes the degree to which air
converges from its surroundings to a point or flows away from a point. It is
used to describe the intensity of divergence and convergence at locations in
space. The formula is as follows.
            <disp-formula id="App1.Ch1.S1.Ex3"><mml:math id="M99" display="block"><mml:mrow><mml:mtext>div</mml:mtext><mml:mi>v</mml:mi><mml:mo>=</mml:mo><mml:mi mathvariant="normal">∇</mml:mi><mml:mo>⋅</mml:mo><mml:mi>v</mml:mi><mml:mo>=</mml:mo><mml:mstyle displaystyle="true"><mml:mfrac style="display"><mml:mrow><mml:mo>∂</mml:mo><mml:msub><mml:mi>u</mml:mi><mml:mi>i</mml:mi></mml:msub></mml:mrow><mml:mrow><mml:mo>∂</mml:mo><mml:msub><mml:mi>x</mml:mi><mml:mi>i</mml:mi></mml:msub></mml:mrow></mml:mfrac></mml:mstyle><mml:mo>=</mml:mo><mml:mstyle displaystyle="true"><mml:mfrac style="display"><mml:mrow><mml:mo>∂</mml:mo><mml:mi>u</mml:mi></mml:mrow><mml:mrow><mml:mo>∂</mml:mo><mml:mi>x</mml:mi></mml:mrow></mml:mfrac></mml:mstyle><mml:mo>+</mml:mo><mml:mstyle displaystyle="true"><mml:mfrac style="display"><mml:mrow><mml:mo>∂</mml:mo><mml:mi>v</mml:mi></mml:mrow><mml:mrow><mml:mo>∂</mml:mo><mml:mi>y</mml:mi></mml:mrow></mml:mfrac></mml:mstyle><mml:mo>+</mml:mo><mml:mstyle displaystyle="true"><mml:mfrac style="display"><mml:mrow><mml:mo>∂</mml:mo><mml:mi>w</mml:mi></mml:mrow><mml:mrow><mml:mo>∂</mml:mo><mml:mi>z</mml:mi></mml:mrow></mml:mfrac></mml:mstyle><mml:mo>,</mml:mo></mml:mrow></mml:math></disp-formula>
          where <inline-formula><mml:math id="M100" display="inline"><mml:mi>u</mml:mi></mml:math></inline-formula>, <inline-formula><mml:math id="M101" display="inline"><mml:mi>v</mml:mi></mml:math></inline-formula>, and <inline-formula><mml:math id="M102" display="inline"><mml:mi>w</mml:mi></mml:math></inline-formula> are the components of the wind in the <inline-formula><mml:math id="M103" display="inline"><mml:mi>x</mml:mi></mml:math></inline-formula>, <inline-formula><mml:math id="M104" display="inline"><mml:mi>y</mml:mi></mml:math></inline-formula>, and <inline-formula><mml:math id="M105" display="inline"><mml:mi>z</mml:mi></mml:math></inline-formula> directions,
respectively. When the <inline-formula><mml:math id="M106" display="inline"><mml:mrow><mml:mtext>div</mml:mtext><mml:mi>v</mml:mi><mml:mo>&lt;</mml:mo><mml:mn mathvariant="normal">0</mml:mn></mml:mrow></mml:math></inline-formula>, the location is
convergence; when the <inline-formula><mml:math id="M107" display="inline"><mml:mrow><mml:mtext>div</mml:mtext><mml:mi>v</mml:mi><mml:mo>&gt;</mml:mo><mml:mn mathvariant="normal">0</mml:mn></mml:mrow></mml:math></inline-formula>, the location is divergence.</p>
</sec>
<sec id="App1.Ch1.S1.SS6">
  <label>A6</label><title>PBLH validation</title>
      <p id="d1e2983">The bulk Richardson number (<italic>Ri</italic>) method was taken to estimate the PBLH based on
the sounding data of Zhengzhou. <italic>Ri</italic> is expressed as
            <disp-formula id="App1.Ch1.S1.Ex4"><mml:math id="M108" display="block"><mml:mrow><mml:mi mathvariant="italic">Ri</mml:mi><mml:mo>(</mml:mo><mml:mi>z</mml:mi><mml:mo>)</mml:mo><mml:mo>=</mml:mo><mml:mstyle displaystyle="true"><mml:mfrac style="display"><mml:mrow><mml:mo>(</mml:mo><mml:mi>g</mml:mi><mml:mo>/</mml:mo><mml:msub><mml:mi mathvariant="italic">θ</mml:mi><mml:mtext>vs</mml:mtext></mml:msub><mml:mo>)</mml:mo><mml:mo>(</mml:mo><mml:msub><mml:mi mathvariant="italic">θ</mml:mi><mml:mtext>vz</mml:mtext></mml:msub><mml:mo>-</mml:mo><mml:msub><mml:mi mathvariant="italic">θ</mml:mi><mml:mtext>vs</mml:mtext></mml:msub><mml:mo>)</mml:mo><mml:mo>(</mml:mo><mml:mi>z</mml:mi><mml:mo>-</mml:mo><mml:msub><mml:mi>z</mml:mi><mml:mi mathvariant="normal">s</mml:mi></mml:msub><mml:mo>)</mml:mo></mml:mrow><mml:mrow><mml:mo>(</mml:mo><mml:msub><mml:mi>u</mml:mi><mml:mi mathvariant="normal">z</mml:mi></mml:msub><mml:mo>-</mml:mo><mml:msub><mml:mi>u</mml:mi><mml:mi mathvariant="normal">s</mml:mi></mml:msub><mml:msup><mml:mo>)</mml:mo><mml:mn mathvariant="normal">2</mml:mn></mml:msup><mml:mo>+</mml:mo><mml:mo>(</mml:mo><mml:msub><mml:mi>v</mml:mi><mml:mi mathvariant="normal">z</mml:mi></mml:msub><mml:mo>-</mml:mo><mml:msub><mml:mi>v</mml:mi><mml:mi mathvariant="normal">s</mml:mi></mml:msub><mml:msup><mml:mo>)</mml:mo><mml:mn mathvariant="normal">2</mml:mn></mml:msup><mml:mo>+</mml:mo><mml:mo>(</mml:mo><mml:mi>b</mml:mi><mml:msubsup><mml:mi>u</mml:mi><mml:mo>∗</mml:mo><mml:mn mathvariant="normal">2</mml:mn></mml:msubsup><mml:mo>)</mml:mo></mml:mrow></mml:mfrac></mml:mstyle><mml:mspace linebreak="nobreak" width="0.33em"/><mml:mo>,</mml:mo></mml:mrow></mml:math></disp-formula>
          where <inline-formula><mml:math id="M109" display="inline"><mml:mi>z</mml:mi></mml:math></inline-formula> is the height above ground, s the surface, <inline-formula><mml:math id="M110" display="inline"><mml:mi>g</mml:mi></mml:math></inline-formula> the acceleration of
gravity, <inline-formula><mml:math id="M111" display="inline"><mml:mrow><mml:msub><mml:mi mathvariant="italic">θ</mml:mi><mml:mi mathvariant="normal">v</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> the virtual potential temperature, <inline-formula><mml:math id="M112" display="inline"><mml:mi>u</mml:mi></mml:math></inline-formula> and <inline-formula><mml:math id="M113" display="inline"><mml:mi>v</mml:mi></mml:math></inline-formula> the
components of wind speed, and <inline-formula><mml:math id="M114" display="inline"><mml:mrow><mml:msub><mml:mi>u</mml:mi><mml:mo>∗</mml:mo></mml:msub></mml:mrow></mml:math></inline-formula> the surface friction velocity.
<inline-formula><mml:math id="M115" display="inline"><mml:mrow><mml:msub><mml:mi>u</mml:mi><mml:mo>∗</mml:mo></mml:msub></mml:mrow></mml:math></inline-formula> can be ignored here due to it being small relative to the wind
shear (Vogelezang and Holtslag, 1996). Previous theoretical and
laboratory studies suggested that when <italic>Ri</italic> is smaller than a critical value
(<inline-formula><mml:math id="M116" display="inline"><mml:mrow><mml:mo>∼</mml:mo><mml:mn mathvariant="normal">0.25</mml:mn></mml:mrow></mml:math></inline-formula>), the laminar flow becomes unstable (Stull, 1988).
Therefore, the lowest level <inline-formula><mml:math id="M117" display="inline"><mml:mi>z</mml:mi></mml:math></inline-formula> at which the interpolated <italic>Ri</italic> exceeds the
critical value of 0.25 is referred to as PBLH in this study, which is
referred to as the criterion used by Seidel et al. (2012). The <inline-formula><mml:math id="M118" display="inline"><mml:mi>R</mml:mi></mml:math></inline-formula> value
is 0.57, passing the 99 % significance test. It can be seen from Fig. A1
that the variation in boundary layer height is generally captured.</p>
</sec>
</app>
  </app-group><notes notes-type="codedataavailability"><title>Code and data availability</title>

      <p id="d1e3212">All source code and data can be accessed by contacting the corresponding
authors Sunling Gong (gongsl@cma.gov.cn) and Lei Zhang (leiz09@cma.gov.cn).</p>
  </notes><notes notes-type="authorcontribution"><title>Author contributions</title>

      <p id="d1e3218">SG and LZ designed the research. HZ performed the
simulations and wrote the manuscript with suggestions from all authors.
JM, HK, XW, and SL assisted with data processing.
JH, YW, JN, and LS participated in the
scientific interpretation and discussion. All authors contributed to the
discussion and improvement of the paper.</p>
  </notes><notes notes-type="competinginterests"><title>Competing interests</title>

      <p id="d1e3224">The contact author has declared that neither they nor their co-authors have any competing interests.</p>
  </notes><notes notes-type="disclaimer"><title>Disclaimer</title>

      <p id="d1e3230">Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.</p>
  </notes><notes notes-type="sistatement"><title>Special issue statement</title>

      <p id="d1e3236">This article is part of the special issue “Air quality research at street level (ACP/GMD inter-journal SI)”. It is not associated with a conference.</p>
  </notes><ack><title>Acknowledgements</title><p id="d1e3242">The authors would like to acknowledge Bin Cui and Lin Zhang from the Peking
University and Liangfu Chen from Chinese Academy of Sciences for their
valuable suggestions to improve the article.</p></ack><notes notes-type="financialsupport"><title>Financial support</title>

      <p id="d1e3247">This research has been supported by the National Natural Science Foundation of China (grant nos. 91744209, 41975131, and 41705080), the CAMS Basis Research Project (grant no. 2019Z009), CAMS Science and Technology Development Fund (grant no. 2018KJ020), and the Atmospheric special integration project (grant no. 2019YFC0214801).</p>
  </notes><notes notes-type="reviewstatement"><title>Review statement</title>

      <p id="d1e3253">This paper was edited by Yang Zhang and reviewed by Sergio Ibarra and one anonymous referee.</p>
  </notes><ref-list>
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