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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>
</journal-title-group>
<issn pub-type="epub">1680-7324</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/acp-12-2263-2012</article-id>
<title-group>
<article-title>Global NO&lt;sub&gt;x&lt;/sub&gt; emission estimates derived from an assimilation of OMI tropospheric NO&lt;sub&gt;2&lt;/sub&gt; columns</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Miyazaki</surname>
<given-names>K.</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 contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Eskes</surname>
<given-names>H. J.</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>Sudo</surname>
<given-names>K.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Royal Netherlands Meteorological Institute (KNMI), Wilhelminalaan 10, 3732 GK, De Bilt, The Netherlands</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Japan Agency for Marine-Earth Science and Technology, Yokohama 236-0001, Japan</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Graduate School of Environmental Studies, Nagoya University, Nagoya, Japan</addr-line>
</aff>
<pub-date pub-type="epub">
<day>01</day>
<month>03</month>
<year>2012</year>
</pub-date>
<volume>12</volume>
<issue>5</issue>
<fpage>2263</fpage>
<lpage>2288</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>
<self-uri xlink:href="http://www.atmos-chem-phys.net/12/2263/2012/acp-12-2263-2012.html">This article is available from http://www.atmos-chem-phys.net/12/2263/2012/acp-12-2263-2012.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/12/2263/2012/acp-12-2263-2012.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/12/2263/2012/acp-12-2263-2012.pdf</self-uri>
<abstract>
<p>A data assimilation system has been developed to estimate global nitrogen
oxides (NO&lt;sub&gt;x&lt;/sub&gt;) emissions using OMI tropospheric NO&lt;sub&gt;2&lt;/sub&gt; columns
(DOMINO product) and a global chemical transport model (CTM), the Chemical
Atmospheric GCM for Study of Atmospheric Environment and Radiative Forcing
(CHASER). The data assimilation system, based on an ensemble Kalman filter
approach, was applied to optimize daily NO&lt;sub&gt;x&lt;/sub&gt; emissions with a
horizontal resolution of 2.8° during the years 2005 and 2006. The
background error covariance estimated from the ensemble CTM forecasts
explicitly represents non-direct relationships between the emissions and
tropospheric columns caused by atmospheric transport and chemical processes.
In comparison to the a priori emissions based on bottom-up inventories, the
optimized emissions were higher over eastern China, the eastern United
States, southern Africa, and central-western Europe, suggesting that the
anthropogenic emissions are mostly underestimated in the inventories. In
addition, the seasonality of the estimated emissions differed from that of
the a priori emission over several biomass burning regions, with a large
increase over Southeast Asia in April and over South America in October. The
data assimilation results were validated against independent data: SCIAMACHY
tropospheric NO&lt;sub&gt;2&lt;/sub&gt; columns and vertical NO&lt;sub&gt;2&lt;/sub&gt; profiles obtained
from aircraft and lidar measurements. The emission correction greatly
improved the agreement between the simulated and observed NO&lt;sub&gt;2&lt;/sub&gt; fields;
this implies that the data assimilation system efficiently derives
NO&lt;sub&gt;x&lt;/sub&gt; emissions from concentration observations. We also demonstrated
that biases in the satellite retrieval and model settings used in the data
assimilation largely affect the magnitude of estimated emissions. These
dependences should be carefully considered for better understanding
NO&lt;sub&gt;x&lt;/sub&gt; sources from top-down approaches.</p>
</abstract>
<counts><page-count count="26"/></counts>
</article-meta>
</front>
<body/>
<back>
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