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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-10-10705-2010</article-id>
<title-group>
<article-title>Some implications of sampling choices on comparisons between satellite and model aerosol optical depth fields</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Sayer</surname>
<given-names>A. 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>Thomas</surname>
<given-names>G. E.</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>Palmer</surname>
<given-names>P. I.</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>Grainger</surname>
<given-names>R. G.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Atmospheric, Oceanic and Planetary Physics, Clarendon Laboratory,  Parks Road, Oxford, OX1 3PU, UK</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Rutherford Appleton Laboratory,  Harwell Science and Innovation Campus, Didcot, OX11 0QX, UK</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>School  of GeoSciences, University of Edinburgh, Edinburgh, EH9 3JW, UK</addr-line>
</aff>
<pub-date pub-type="epub">
<day>16</day>
<month>11</month>
<year>2010</year>
</pub-date>
<volume>10</volume>
<issue>22</issue>
<fpage>10705</fpage>
<lpage>10716</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/10/10705/2010/acp-10-10705-2010.html">This article is available from http://www.atmos-chem-phys.net/10/10705/2010/acp-10-10705-2010.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/10/10705/2010/acp-10-10705-2010.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/10/10705/2010/acp-10-10705-2010.pdf</self-uri>
<abstract>
<p>The comparison of satellite and model aerosol optical depth (AOD)
      fields provides useful information on the strengths and weaknesses of
      both. However, the sampling of satellite and models is very different
      and some subjective decisions about data selection and aggregation
      must be made in order to perform such comparisons. This work examines
      some implications of these decisions, using GlobAerosol AOD retrievals
      at 550 nm from Advanced Along-Track Scanning Radiometer
      (AATSR) measurements, and aerosol fields from the GEOS-Chem chemistry
      transport model. It is recommended to sample the model only where the
      satellite flies over on a particular day; neglecting this can cause
      regional differences in model AOD of up to 0.1 on monthly and annual
      timescales. The comparison is observed to depend strongly upon
      thresholds for sparsity of satellite retrievals in the model grid
      cells. Requiring at least 25% coverage of the model grid cell by
      satellite data decreases the observed difference between the two by
      approximately half over land. The impact over ocean is smaller. In
      both model and satellite datasets, there is an anticorrelation between
      the proportion &lt;i&gt;p&lt;/i&gt; of a model grid cell covered by satellite
      retrievals and the AOD. This is attributed to small &lt;i&gt;p&lt;/i&gt; typically
      occuring due to high cloud cover and lower AODs being found in large
      clear-sky regions. Daily median AATSR AODs were found to be closer to
      GEOS-Chem AODs than daily means (with the root mean squared difference
      being approximately 0.05 smaller). This is due to the decreased
      sensitivity of medians to outliers such as cloud-contaminated
      retrievals, or aerosol point sources not included in the model.</p>
</abstract>
<counts><page-count count="12"/></counts>
</article-meta>
</front>
<body/>
<back>
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