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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ACP</journal-id>
<journal-title-group>
<journal-title>Atmospheric Chemistry and Physics</journal-title>
<abbrev-journal-title abbrev-type="publisher">ACP</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Atmos. Chem. Phys.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7324</issn>
<publisher><publisher-name>Copernicus Publications</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acp-14-11247-2014</article-id>
<title-group>
<article-title>Aerosol indirect effect on the grid-scale clouds in the two-way coupled WRF–CMAQ: model description, development, evaluation and regional analysis</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Yu</surname>
<given-names>S.</given-names>
<ext-link>https://orcid.org/0000-0001-9718-8246</ext-link>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Mathur</surname>
<given-names>R.</given-names>
<ext-link>https://orcid.org/0000-0001-8927-5876</ext-link>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Pleim</surname>
<given-names>J.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Wong</surname>
<given-names>D.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Gilliam</surname>
<given-names>R.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Alapaty</surname>
<given-names>K.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Zhao</surname>
<given-names>C.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Liu</surname>
<given-names>X.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Research Center for Air Pollution and Health, College of Environmental and Resource Sciences, Zhejiang University, Hangzhou, Zhejiang 310058, P.R. China</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Atmospheric Modeling and Analysis Division, National Exposure Research Laboratory, US Environmental Protection Agency, Research Triangle Park, NC 27711, USA</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Atmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory, Richland, WA 99352, USA</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>now at: Department of Atmospheric Science, University of Wyoming, Laramie, WY 82071, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>24</day>
<month>10</month>
<year>2014</year>
</pub-date>
<volume>14</volume>
<issue>20</issue>
<fpage>11247</fpage>
<lpage>11285</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2014 S. Yu et al.</copyright-statement>
<copyright-year>2014</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 3.0 Unported License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by/3.0/">https://creativecommons.org/licenses/by/3.0/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://acp.copernicus.org/articles/14/11247/2014/acp-14-11247-2014.html">This article is available from https://acp.copernicus.org/articles/14/11247/2014/acp-14-11247-2014.html</self-uri>
<self-uri xlink:href="https://acp.copernicus.org/articles/14/11247/2014/acp-14-11247-2014.pdf">The full text article is available as a PDF file from https://acp.copernicus.org/articles/14/11247/2014/acp-14-11247-2014.pdf</self-uri>
<abstract>
<p>This study implemented first, second and glaciation aerosol indirect effects
(AIE) on resolved clouds in the two-way coupled Weather Research and
Forecasting Community Multiscale Air Quality (WRF–CMAQ) modeling system by
including parameterizations for both cloud drop and ice number concentrations
on the basis of CMAQ-predicted aerosol distributions and WRF meteorological
conditions. The performance of the newly developed WRF–CMAQ model, with
alternate Community Atmospheric Model (CAM) and Rapid Radiative Transfer
Model for GCMs (RRTMG) radiation schemes, was evaluated with observations
from the Clouds and the See &lt;a href=&quot;http://ceres.larc.nasa.gov/&quot;target=&quot;_blank&quot;&gt;http://ceres.larc.nasa.gov/&lt;/a&gt;.
Earth&apos;s Radiant Energy System (CERES) satellite and surface monitoring
networks (AQS, IMPROVE, CASTNET, STN, and PRISM) over the continental US
(CONUS) (12 km resolution) and eastern Texas (4 km resolution) during
August and September of 2006. The results at the Air Quality System (AQS)
surface sites show that in August, the normalized mean bias (NMB) values for
PM&lt;sub&gt;2.5&lt;/sub&gt; over the eastern US (EUS) and the western US (WUS) are 5.3%
(−0.1%) and 0.4% (−5.2%) for WRF–CMAQ/CAM
(WRF–CMAQ/RRTMG), respectively. The evaluation of PM&lt;sub&gt;2.5&lt;/sub&gt; chemical
composition reveals that in August, WRF–CMAQ/CAM (WRF–CMAQ/RRTMG)
consistently underestimated the observed SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;2-&lt;/sup&gt; by −23.0%
(−27.7%), −12.5% (−18.9%) and −7.9%
(−14.8%) over the EUS at the Clean Air Status Trends Network
(CASTNET), Interagency Monitoring of Protected Visual Environments (IMPROVE) and
Speciated Trends Network (STN) sites, respectively. Both configurations
(WRF–CMAQ/CAM, WRF–CMAQ/RRTMG) overestimated the observed mean organic
carbon (OC), elemental carbon (EC) and and total carbon (TC) concentrations
over the EUS in August at the IMPROVE sites. Both configurations generally
underestimated the cloud field (shortwave cloud forcing, SWCF) over the CONUS
in August due to the fact that the AIE on the subgrid convective clouds was
not considered when the model simulations were run at the 12 km resolution.
This is in agreement with the fact that both configurations captured SWCF and
longwave cloud forcing (LWCF) very well for the 4 km simulation over eastern
Texas, when all clouds were resolved by the finer resolution domain. The
simulations of WRF–CMAQ/CAM and WRF–CMAQ/RRTMG show dramatic improvements
for SWCF, LWCF, cloud optical depth (COD), cloud fractions and precipitation
over the ocean relative to those of WRF default cases in August. The model
performance in September is similar to that in August, except for a greater
overestimation of PM&lt;sub&gt;2.5&lt;/sub&gt; due to the overestimations of SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;2-&lt;/sup&gt;,
NH&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;+&lt;/sup&gt;, NO&lt;sub&gt;3&lt;/sub&gt;&lt;sup&gt;-&lt;/sup&gt;, and TC over the EUS, less underestimation of
clouds (SWCF) over the land areas due to the lower SWCF values, and fewer
convective clouds in September. This work shows that inclusion of indirect
aerosol effect treatments in WRF–CMAQ represents a significant advancement
and milestone in air quality modeling and the development of integrated
emissions control strategies for air quality management and climate change
mitigation.</p>
</abstract>
<counts><page-count count="39"/></counts>
</article-meta>
</front>
<body/>
<back>
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