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<article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" article-type="research-article" dtd-version="3.0" xml:lang="en">
<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-12-4279-2012</article-id>
<title-group>
<article-title>A tropospheric ozone maximum over the equatorial Southern Indian Ocean</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Zhang</surname>
<given-names>L.</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>Li</surname>
<given-names>Q. B.</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>Murray</surname>
<given-names>L. T.</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>Luo</surname>
<given-names>M.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Liu</surname>
<given-names>H.</given-names>
</name>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Jiang</surname>
<given-names>J. H.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Mao</surname>
<given-names>Y.</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>Chen</surname>
<given-names>D.</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>Gao</surname>
<given-names>M.</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>Livesey</surname>
<given-names>N.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Department of Atmospheric and Oceanic Sciences, University of California, Los Angeles, CA, USA</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Joint Institute for Regional Earth System Science and Engineering, University of California, Los Angeles, CA, USA</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>School of Engineering and Applied Sciences, Harvard University, Cambridge, MA, USA</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Jet Propulsion Laboratory, California Institute of Technology, CA, USA</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>National Institute of Aerospace, Hampton, VA, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>14</day>
<month>05</month>
<year>2012</year>
</pub-date>
<volume>12</volume>
<issue>9</issue>
<fpage>4279</fpage>
<lpage>4296</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/12/4279/2012/acp-12-4279-2012.html">This article is available from http://www.atmos-chem-phys.net/12/4279/2012/acp-12-4279-2012.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/12/4279/2012/acp-12-4279-2012.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/12/4279/2012/acp-12-4279-2012.pdf</self-uri>
<abstract>
<p>We examine the distribution of tropical tropospheric ozone (O&lt;sub&gt;3&lt;/sub&gt;) from
the Microwave Limb Sounder (MLS) and the Tropospheric Emission Spectrometer
(TES) by using a global three-dimensional model of tropospheric chemistry
(GEOS-Chem). MLS and TES observations of tropospheric O&lt;sub&gt;3&lt;/sub&gt; during 2005 to
2009 reveal a distinct, persistent O&lt;sub&gt;3&lt;/sub&gt; maximum, both in mixing ratio and
tropospheric column, in May over the Equatorial Southern Indian Ocean
(ESIO). The maximum is most pronounced in 2006 and 2008 and less evident in
the other three years. This feature is also consistent with the total column
O&lt;sub&gt;3&lt;/sub&gt; observations from the Ozone Mapping Instrument (OMI) and the
Atmospheric Infrared Sounder (AIRS). Model results reproduce the observed
May O&lt;sub&gt;3&lt;/sub&gt; maximum and the associated interannual variability. The origin
of the maximum reflects a complex interplay of chemical and dynamic factors.
The O&lt;sub&gt;3&lt;/sub&gt; maximum is dominated by the O&lt;sub&gt;3&lt;/sub&gt; production driven by
lightning nitrogen oxides (NO&lt;sub&gt;x&lt;/sub&gt;) emissions, which accounts for 62% of
the tropospheric column O&lt;sub&gt;3&lt;/sub&gt; in May 2006. We find the contribution from
biomass burning, soil, anthropogenic and biogenic sources to the O&lt;sub&gt;3&lt;/sub&gt;
maximum are rather small. The O&lt;sub&gt;3&lt;/sub&gt; productions in the lightning outflow
from Central Africa and South America both peak in May and are directly
responsible for the O&lt;sub&gt;3&lt;/sub&gt; maximum over the western ESIO. The lightning
outflow from Equatorial Asia dominates over the eastern ESIO. The
interannual variability of the O&lt;sub&gt;3&lt;/sub&gt; maximum is driven largely by the
anomalous anti-cyclones over the southern Indian Ocean in May 2006 and
2008. The lightning outflow from Central Africa and South America is
effectively entrained by the anti-cyclones followed by northward transport
to the ESIO.</p>
</abstract>
<counts><page-count count="18"/></counts>
</article-meta>
</front>
<body/>
<back>
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