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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-11-11647-2011</article-id>
<title-group>
<article-title>Effects of model resolution on the interpretation of satellite NO&lt;sub&gt;2&lt;/sub&gt; observations</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Valin</surname>
<given-names>L. C.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Russell</surname>
<given-names>A. R.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Hudman</surname>
<given-names>R. C.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Cohen</surname>
<given-names>R. C.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>College of Chemistry, University of California Berkeley, Berkeley, CA 94720, USA</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Department of Earth and Planetary Sciences, University of California Berkeley, Berkeley, CA 94720, USA</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>now at: Environmental Protection Agency, Region 9, San Francisco, CA 94105, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>22</day>
<month>11</month>
<year>2011</year>
</pub-date>
<volume>11</volume>
<issue>22</issue>
<fpage>11647</fpage>
<lpage>11655</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2011 L. C. Valin et al.</copyright-statement>
<copyright-year>2011</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/11/11647/2011/acp-11-11647-2011.html">This article is available from https://acp.copernicus.org/articles/11/11647/2011/acp-11-11647-2011.html</self-uri>
<self-uri xlink:href="https://acp.copernicus.org/articles/11/11647/2011/acp-11-11647-2011.pdf">The full text article is available as a PDF file from https://acp.copernicus.org/articles/11/11647/2011/acp-11-11647-2011.pdf</self-uri>
<abstract>
<p>Inference of NO&lt;sub&gt;x&lt;/sub&gt; emissions (NO+NO&lt;sub&gt;2&lt;/sub&gt;) from satellite observations
of tropospheric NO&lt;sub&gt;2&lt;/sub&gt; column requires knowledge of NO&lt;sub&gt;x&lt;/sub&gt; lifetime,
usually provided by chemical transport models (CTMs). However, it is known
that species subject to non-linear sources or sinks, such as ozone, are
susceptible to biases in coarse-resolution CTMs. Here we compute the
resolution-dependent bias in predicted NO&lt;sub&gt;2&lt;/sub&gt; column, a quantity relevant to
the interpretation of space-based observations. We use 1-D and 2-D models to
illustrate the mechanisms responsible for these biases over a range of NO&lt;sub&gt;2&lt;/sub&gt;
concentrations and model resolutions. We find that predicted biases are
largest at coarsest model resolutions with negative biases predicted over
large sources and positive biases predicted over small sources. As an
example, we use WRF-CHEM to illustrate the resolution necessary to predict 
10 AM and 1 PM NO&lt;sub&gt;2&lt;/sub&gt; column to 10 and 25% accuracy over three large sources,
the Four Corners power plants in NW New Mexico, Los Angeles, and the San
Joaquin Valley in California for a week-long simulation in July 2006. We find
that resolution in the range of 4–12 km is sufficient to accurately model
nonlinear effects in the NO&lt;sub&gt;2&lt;/sub&gt; loss rate.</p>
</abstract>
<counts><page-count count="9"/></counts>
</article-meta>
</front>
<body/>
<back>
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