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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>
</journal-title-group>
<issn pub-type="epub">1680-7375</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/acpd-11-8027-2011</article-id>
<title-group>
<article-title>Simulation of the mineral dust content over Western Africa with the CHIMERE-DUST model from the event to the annual scale</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Schmechtig</surname>
<given-names>C.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Marticorena</surname>
<given-names>B.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Chatenet</surname>
<given-names>B.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Bergametti</surname>
<given-names>G.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Rajot</surname>
<given-names>J. L.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>LISA, UMR CNRS 7583, Universités Paris Est-Paris Diderot, Créteil, France</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>IRD-UMR 211 BIOEMCO, Niamey, Niger</addr-line>
</aff>
<pub-date pub-type="epub">
<day>09</day>
<month>03</month>
<year>2011</year>
</pub-date>
<volume>11</volume>
<issue>3</issue>
<fpage>8027</fpage>
<lpage>8079</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>
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<abstract>
<p>The chemistry and transport model CHIMERE-Dust have been used to simulate
the mineral dust cycle over the Sahara in 2006. Surface measurements
deployed during the AMMA field campaign allows to test the capability of the
model to correctly reproduce the atmospheric dust load and surface
concentrations from the daily to the seasonal time-scale. The seasonal
pattern simulated for Aerosol Optical Depth and surface concentrations are
in good agreement with observations. The simulated daily concentrations and
hourly AOD are in the same range than the observed one despite relatively
high simulated dust emissions. At the different time-scales, the
quantitative agreement between the simulations and the observations is
fairly good. The capability of the model to reproduce the altitude of the
dust transport was tested for two contrasted cases of low and high altitude
transport. These results highlights the sensitivity of the simulations to
the surface winds used as external forcing and the necessity to further
constrain the dust mass budget at the regional scale.</p>
</abstract>
<counts><page-count count="53"/></counts>
</article-meta>
</front>
<body/>
<back>
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