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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ACPD</journal-id>
<journal-title-group>
<journal-title>Atmospheric Chemistry and Physics Discussions</journal-title>
<abbrev-journal-title abbrev-type="publisher">ACPD</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Atmos. Chem. Phys. Discuss.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7375</issn>
<publisher><publisher-name></publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acpd-10-3053-2010</article-id>
<title-group>
<article-title>Impacts of dust on West African climate during 2005 and 2006</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Camara</surname>
<given-names>M.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Jenkins</surname>
<given-names>G.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Konare</surname>
<given-names>A.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Département de Physique, Université de Ziguinchor, BP 523, Ziguinchor, Senegal</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Physics and astronomy department, Howard University, DC, 20059, USA</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Université de Cocody, Abidjan 22, BP 582, Côte d&apos;Ivoire</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Laboratoire de Physique de l&apos;atmosphère &amp;ndash; SF, BP 5085 Dakar-Fann, Senegal</addr-line>
</aff>
<pub-date pub-type="epub">
<day>05</day>
<month>02</month>
<year>2010</year>
</pub-date>
<volume>10</volume>
<issue>2</issue>
<fpage>3053</fpage>
<lpage>3086</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2010 M. Camara et al.</copyright-statement>
<copyright-year>2010</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 3.0 Unported License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by/3.0/">https://creativecommons.org/licenses/by/3.0/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://acp.copernicus.org/preprints/10/3053/2010/acpd-10-3053-2010.html">This article is available from https://acp.copernicus.org/preprints/10/3053/2010/acpd-10-3053-2010.html</self-uri>
<self-uri xlink:href="https://acp.copernicus.org/preprints/10/3053/2010/acpd-10-3053-2010.pdf">The full text article is available as a PDF file from https://acp.copernicus.org/preprints/10/3053/2010/acpd-10-3053-2010.pdf</self-uri>
<abstract>
<p>The aim of this study is to understand the impacts of Saharan dust
      outbreaks on West African climate using a 3-dimensional, hydrostatic,
      sigma vertical coordinate regional climate model (RegCM). We performed
      a simulation with the non aerosol version of the model (control case)
      followed by another simulation using the desert dust module (dust
      case) implemented in RegCM which includes emission, transport,
      gravitational settling, wet and dry removal and calculation of dust
      optical properties for 2005 and 2006. Dynamic and thermodynamic
      parameters obtained from both versions of the model are intercompared
      and validated with NCEP/NCAR reanalysis, African Monsoon
      Multidisciplinary Analysis (AMMA) program data and the Global
      Precipitation Climatology Project (GPCP) rainfall products. The
      spatial and temporal distribution of the Aerosol optical depth derived
      from the desert dust run is compared to available observed aerosol
      data such as the Aerosol Robotic Network (AERONET) program and
      satellites data.
&lt;br&gt;&lt;br&gt;
      Using radiosounding data and RegCM outputs, a case study of a strong
      dust outbreak showed the presence of a stable environment at Dakar,
      Sal and Nouadhibou stations.</p>
</abstract>
<counts><page-count count="34"/></counts>
</article-meta>
</front>
<body/>
<back>
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</article>