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<article language="en">
	<journal>
		<journal_title>Atmospheric Chemistry and Physics Discussions</journal_title>
		<journal_url>www.atmos-chem-phys-discuss.net</journal_url>
		<issn>1680-7367</issn>
		<eissn>1680-7375</eissn>
		<volume_number>8</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/acpd-8-6469-2008</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/8/6469/2008/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/8/6469/2008/acpd-8-6469-2008.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/8/6469/2008/acpd-8-6469-2008.pdf</fulltext_pdf>
	<start_page>6469</start_page>
	<end_page>6499</end_page>
	<publication_date>2008-04-01</publication_date>
	<article_title content_type="html">A method for evaluating spatially-resolved NO&lt;sub&gt;x&lt;/sub&gt; emissions using Kalman filter inversion, direct sensitivities, and space-based NO&lt;sub&gt;2&lt;/sub&gt; observations</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>S. L. Napelenok</name>
			<email>napelenok.sergey@epa.gov</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>R. W. Pinder</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>A. B. Gilliland</name>
		</author>
		<author numeration="4" affiliations="2,3">
			<name>R. V. Martin</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Atmospheric Sciences Modeling Division, Air Resources Laboratory, National Oceanic and Atmospheric Administration, in partnership with the United States Environmental Protection Agency, 109 T.W. Alexander Drive, Research Triangle Park, NC 27711, USA</affiliation>
		<affiliation numeration="2" content_type="html">Department of Physics and Atmospheric Science, Dalhousie University, Halifax, NS, Canada</affiliation>
		<affiliation numeration="3" content_type="html">Harvard-Smithsonian Center for Astrophysics, Cambridge, MA, USA</affiliation>
	</affiliations>
	<abstract content_type="html">An inverse modeling method was developed and tested for identifying possible
biases in emission inventories using satellite observations. The
relationships between emission inputs and modeled ambient concentrations
were estimated using sensitivities calculated with the decoupled direct
method in three dimensions (DDM-3D) implemented within the framework of the
Community Multiscale Air Quality (CMAQ) regional model. As a case study to
test the approach, the method was applied to regional ground-level NO&lt;sub&gt;x&lt;/sub&gt;
emissions in the southeastern United States as constrained by the Scanning
Imaging Absorption Spectrometer for Atmospheric Chartography (SCIAMACHY)
satellite derived observations of NO&lt;sub&gt;2&lt;/sub&gt; column densities. A controlled
&quot;pseudodata&quot; scenario with a known solution was used to establish that the
methodology can achieve the correct solution, and the approach was then
applied to a summer 2004 period where the satellite data are available. The
results indicate that emissions biases differ in urban and rural areas of
the southeast. The method suggested slight downward (less than 10%)
adjustment to urban emissions, while rural region results were found to be
highly sensitive to NO&lt;sub&gt;x&lt;/sub&gt; processes in the upper troposphere. As such,
the bias in the rural areas is likely not solely due to biases in the
ground-level emissions. It was found that CMAQ was unable to predict the
significant level of NO&lt;sub&gt;2&lt;/sub&gt; in the upper troposphere that was observed
during the NASA Intercontinental Chemical Transport Experiment (INTEX)
measurement campaign. The reasons for the underestimation likely include
combination of a lack of lightning emissions and a short modeled lifetime of
NO&lt;sub&gt;x&lt;/sub&gt; aloft. Therefore, the best correlation between satellite
observations and modeled NO&lt;sub&gt;2&lt;/sub&gt; column densities, as well as comparison to
ground-level observations of NO&lt;sub&gt;2&lt;/sub&gt;, was obtained from performing the
inverse while accounting for the significant presence of NO&lt;sub&gt;2&lt;/sub&gt; in the
upper troposphere not captured by the regional model.</abstract>
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</article>

