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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-9-6157-2009</article-id>
<title-group>
<article-title>An overview of two years of ozone radio soundings over Cotonou as part of AMMA</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Thouret</surname>
<given-names>V.</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>Saunois</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>Minga</surname>
<given-names>A.</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>Mariscal</surname>
<given-names>A.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff7">
<sup>7</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Sauvage</surname>
<given-names>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>Solete</surname>
<given-names>A.</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>Agbangla</surname>
<given-names>D.</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>Nédélec</surname>
<given-names>P.</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>Mari</surname>
<given-names>C.</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>Reeves</surname>
<given-names>C. E.</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>Schlager</surname>
<given-names>H.</given-names>
</name>
<xref ref-type="aff" rid="aff6">
<sup>6</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Université de Toulouse, UPS, LA (Laboratoire d&apos;Aérologie), 14 avenue Edouard Belin, 31400, Toulouse, France</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>CNRS, LA (Laboratoire d&apos;Aérologie), 31400 Toulouse, France</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Faculté des Sciences, Université Marien NGouabi, BP 2702 Brazzaville, Congo</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Agence pour la SECurité de la Navigation Aérienne en Afrique et à Madagascar (ASECNA), BP 96, Cotonou, Benin</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>School of Environmental Sciences, University of East Anglia, Norwich, NR4 7TJ, UK</addr-line>
</aff>
<aff id="aff6">
<label>6</label>
<addr-line>Deutsches Zentrum fuer Luft-und Raumfahrt (DLR), Institut fuer Physik der Atmosphaere, Oberpfaffenhofen, 82234 Wessling, Germany</addr-line>
</aff>
<aff id="aff7">
<label>7</label>
<addr-line>now at: LGIT (Laboratoire de Géophysique Interne et Technophysique), BP 53, 38 041 Grenoble, Cedex 09, France</addr-line>
</aff>
<pub-date pub-type="epub">
<day>28</day>
<month>08</month>
<year>2009</year>
</pub-date>
<volume>9</volume>
<issue>16</issue>
<fpage>6157</fpage>
<lpage>6174</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/9/6157/2009/acp-9-6157-2009.html">This article is available from http://www.atmos-chem-phys.net/9/6157/2009/acp-9-6157-2009.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/9/6157/2009/acp-9-6157-2009.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/9/6157/2009/acp-9-6157-2009.pdf</self-uri>
<abstract>
<p>As part of the African Monsoon Multidisciplinary Analysis (AMMA) program, a total
of 98 ozone vertical profiles over Cotonou, Benin, have been measured during a
26 month period (December 2004–January 2007). These regular measurements
broadly document the seasonal and interannual variability of ozone in both
the troposphere and the lower stratosphere over West Africa for the first time.
This data set is complementary to the MOZAIC observations made from Lagos between
0 and 12 km during the period 1998–2004. Both data sets highlight the unique
way in which West Africa is impacted by two biomass burning seasons: in
December–February (dry season) due to burning in the Sahelian band and in
June-August (wet season) due to burning in southern Africa. High interannual
variabilities between Cotonou and Lagos data sets and within each data set are
observed and are found to be a major characteristic of this region. In particular,
the dry and wet seasons are discussed in order to set the data of the Special
Observing Periods (SOPs) into a climatological context. Compared to other dry
and wet seasons, the 2006 dry and wet season campaigns took place in rather
high ozone environments. During the sampled wet seasons, southern intrusions
of biomass burning were particularly frequent with concentrations up to 120 ppbv
of ozone in the lower troposphere. An insight into the ozone distribution in
the upper troposphere and the lower stratosphere (up to 26 km) is given. The
first tropospheric columns of ozone based on in-situ data over West Africa are
assessed. They compare well with satellite products on seasonal and interannual
time-scales, provided that the layer below 850 hPa where the remote instrument
is less sensitive to ozone, is removed.</p>
</abstract>
<counts><page-count count="18"/></counts>
</article-meta>
</front>
<body/>
<back>
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