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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>GÃ¶ttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acp-9-783-2009</article-id>
<title-group>
<article-title>Methane plume over south Asia during the monsoon season: satellite observation and model simulation</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Xiong</surname>
<given-names>X.</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>Houweling</surname>
<given-names>S.</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>Wei</surname>
<given-names>J.</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>Maddy</surname>
<given-names>E.</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>Sun</surname>
<given-names>F.</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>Barnet</surname>
<given-names>C.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>NOAA/NESDIS/Center for Satellite Applications and Research, Camp Springs, Maryland, USA</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Perot Systems Government Services, Fairfax, Virginia, USA</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Netherlands Institute for Space Research, Utrecht, The Netherlands</addr-line>
</aff>
<pub-date pub-type="epub">
<day>02</day>
<month>02</month>
<year>2009</year>
</pub-date>
<volume>9</volume>
<issue>3</issue>
<fpage>783</fpage>
<lpage>794</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/9/783/2009/acp-9-783-2009.html">This article is available from http://www.atmos-chem-phys.net/9/783/2009/acp-9-783-2009.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/9/783/2009/acp-9-783-2009.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/9/783/2009/acp-9-783-2009.pdf</self-uri>
<abstract>
<p>Satellite retrievals of methane (CH&lt;sub&gt;4&lt;/sub&gt;) using the Atmospheric Infrared
Sounder (AIRS) on the EOS/Aqua platform from 2003â€“2007 show a strong,
plume-like enhancement of CH&lt;sub&gt;4&lt;/sub&gt; in the middle to upper troposphere over
South Asia during July, August and September, with the maximum occurring
in early September. Simulations using the global tracer model version 3
(TM3) also show similar seasonal enhancement of CH&lt;sub&gt;4&lt;/sub&gt; in the same region.
The model results also suggest that this enhancement is associated with
transport processes and local surface emissions, thus the observations of
tropospheric CH&lt;sub&gt;4&lt;/sub&gt; during the monsoon season may be used to constrain the
models for a better estimation of Asian CH&lt;sub&gt;4&lt;/sub&gt; sources. Further
comparisons between the AIRS retrievals and the model simulations suggest a
possible overestimate of emissions from rice paddies in Southeast Asia in
the scenario with the global emissions from rice of 60 Tg yr&lt;sup&gt;&amp;minus;1&lt;/sup&gt;.
Moreover, the observed tropospheric CH&lt;sub&gt;4&lt;/sub&gt; enhancement from AIRS provides
evidence for the strong transport of atmospheric pollutants from the lower
to the upper troposphere in Asia during the monsoon season. The observed
rapid disappearance of the local CH&lt;sub&gt;4&lt;/sub&gt; maximum in September may provide
valuable information for studying the dissipation of the Tibetan anticyclone
and the withdrawal of monsoon.</p>
</abstract>
<counts><page-count count="12"/></counts>
</article-meta>
</front>
<body/>
<back>
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