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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ACPD</journal-id>
<journal-title-group>
<journal-title>Atmospheric Chemistry and Physics Discussions</journal-title>
<abbrev-journal-title abbrev-type="publisher">ACPD</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7375</issn>
<publisher><publisher-name>Copernicus GmbH</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acpd-8-15031-2008</article-id>
<title-group>
<article-title>Inverse modeling and mapping US air quality influences of inorganic PM&lt;sub&gt;2.5&lt;/sub&gt; precursor emissions using the adjoint of GEOS-Chem</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Henze</surname>
<given-names>D. K.</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>Seinfeld</surname>
<given-names>J. H.</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>Shindell</surname>
<given-names>D. T.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Earth Institute, Columbia University, New York, NY, USA</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Division of Chemistry and Chemical Engineering, California Institute of Technology, Pasadena, CA, USA</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>NASA Goddard Institute for Space Studies, New York, NY, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>08</day>
<month>08</month>
<year>2008</year>
</pub-date>
<volume>8</volume>
<issue>4</issue>
<fpage>15031</fpage>
<lpage>15099</lpage>
<permissions>
<license xlink:type="simple">
<license-p>This is an open-access article ditributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.</license-p>
</license>
</permissions>
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<self-uri xlink:href="http://www.atmos-chem-phys-discuss.net/8/15031/2008/acpd-8-15031-2008.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys-discuss.net/8/15031/2008/acpd-8-15031-2008.pdf</self-uri>
<abstract>
<p>Influences of specific sources of inorganic PM&lt;sub&gt;2.5&lt;/sub&gt; on peak and ambient
aerosol concentrations in the US are evaluated using a combination of inverse
modeling and sensitivity analysis. First, sulfate and nitrate aerosol
measurements from the IMPROVE network are assimilated using the
four-dimensional variational (4D-Var) method into the GEOS-Chem chemical
transport model in order to constrain emissions estimates in four separate
month-long inversions (one per season). Of the precursor emissions, these
observations primarily constrain ammonia (NH&lt;sub&gt;3&lt;/sub&gt;). While the net result is a
decrease in estimated US NH&lt;sub&gt;3&lt;/sub&gt; emissions relative to the original inventory,
there is considerable variability in adjustments made to NH&lt;sub&gt;3&lt;/sub&gt; emissions in
different locations, seasons and source sectors, such as focused decreases in
the midwest during July, broad decreases throughout the US~in January,
increases in eastern coastal areas in April, and an effective redistribution
of emissions from natural to anthropogenic sources. Implementing these
constrained emissions, the adjoint model is applied to quantify the
influences of emissions on representative PM&lt;sub&gt;2.5&lt;/sub&gt; air quality metrics
within the US. The resulting sensitivity maps display a wide range of
spatial, sectoral and seasonal variability in the susceptibility of the air
quality metrics to absolute emissions changes and the effectiveness of
incremental emissions controls of specific source sectors. NH&lt;sub&gt;3&lt;/sub&gt; emissions
near sources of sulfur oxides (SO&lt;sub&gt;x&lt;/sub&gt;) are estimated to most influence
peak inorganic PM&lt;sub&gt;2.5&lt;/sub&gt; levels in the East; thus, the most effective
controls of NH&lt;sub&gt;3&lt;/sub&gt; emissions are often disjoint from locations of peak NH&lt;sub&gt;3&lt;/sub&gt;
emissions. Controls of emissions from industrial sectors of SO&lt;sub&gt;x&lt;/sub&gt; and
NO&lt;sub&gt;x&lt;/sub&gt; are estimated to be more effective than surface emissions, and
changes to NH&lt;sub&gt;3&lt;/sub&gt; emissions in regions dominated by natural sources are
disproportionately more effective than regions dominated by anthropogenic
sources. NO&lt;sub&gt;x&lt;/sub&gt; controls are most effective in northern states in
October; in January, SO&lt;sub&gt;x&lt;/sub&gt; controls may be counterproductive. When
considering ambient inorganic PM&lt;sub&gt;2.5&lt;/sub&gt; concentrations, intercontinental
influences are small, though transboundary influences within North America
are significant, with SO&lt;sub&gt;x&lt;/sub&gt; emissions from surface sources in Mexico
contributing almost a fourth of the total influence from this sector.</p>
</abstract>
<counts><page-count count="69"/></counts>
</article-meta>
</front>
<body/>
<back>
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