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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>9</volume_number>
		<issue_number>3</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/acpd-9-11221-2009</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/9/11221/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/9/11221/2009/acpd-9-11221-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/9/11221/2009/acpd-9-11221-2009.pdf</fulltext_pdf>
	<start_page>11221</start_page>
	<end_page>11268</end_page>
	<publication_date>2009-05-05</publication_date>
	<article_title content_type="html">Two years of Ozone radio soundings over Cotonou as part of AMMA: overview</article_title>
	<authors>
		<author numeration="1" affiliations="1,2">
			<name>V. Thouret</name>
			<email>valerie.thouret@aero.obs-mip.fr</email>
		</author>
		<author numeration="2" affiliations="1,2">
			<name>M. Saunois</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>A. Minga</name>
		</author>
		<author numeration="4" affiliations="1,2,7">
			<name>A. Mariscal</name>
		</author>
		<author numeration="5" affiliations="1,2">
			<name>B. Sauvage</name>
		</author>
		<author numeration="6" affiliations="4">
			<name>A. Solete</name>
		</author>
		<author numeration="7" affiliations="4">
			<name>D. Agbangla</name>
		</author>
		<author numeration="8" affiliations="1,2">
			<name>P. Nédélec</name>
		</author>
		<author numeration="9" affiliations="1,2">
			<name>C. Mari</name>
		</author>
		<author numeration="10" affiliations="5">
			<name>C. E. Reeves</name>
		</author>
		<author numeration="11" affiliations="6">
			<name>H. Schlager</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Université de Toulouse, UPS, LA (Laboratoire d&apos;Aérologie), 14  avenue Edouard Belin, 31400, Toulouse, France</affiliation>
		<affiliation numeration="2" content_type="html">CNRS, LA (Laboratoire d&apos;Aérologie), 31400 Toulouse, France</affiliation>
		<affiliation numeration="3" content_type="html">Faculté des Sciences, Université Marien NGouabi, BP 2702  Brazzaville, Congo</affiliation>
		<affiliation numeration="4" content_type="html">Agence pour la SECurité de la Navigation Aérienne en Afrique et à Madagascar (ASECNA), BP 96, Cotonou, Benin</affiliation>
		<affiliation numeration="5" content_type="html">School of Environmental Sciences, University of East Anglia,  Norwich, NR4 7TJ, UK</affiliation>
		<affiliation numeration="6" content_type="html">Deutsches Zentrum fuer Luft-und Raumfahrt (DLR), Institut für  Physik der Atmosphäre, Oberpfaffenhofen, 82234 Wessling, Germany</affiliation>
		<affiliation numeration="7" content_type="html">now at: LGIT (Laboratoire de Géophysique Interne et Technophysique), BP 53, 38 041 Grenoble,  Cedex 09, France</affiliation>
	</affiliations>
	<abstract content_type="html">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
      inter annual 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 inter annual 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 dry and wet season
      campaigns took place in rather high ozoneenvironments. 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 in this region are assessed. They compare well with
      satellite products on seasonal and inter annual time-scales, provided
      that the layer below 850 Pa where the remote instrument is
      less sensitive to ozone, is removed.</abstract>
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