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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-10-25619-2010</article-id>
<title-group>
<article-title>Global retrieval of ATSR cloud parameters and evaluation (GRAPE): dataset assessment</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>Poulsen</surname>
<given-names>C. A.</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>Arnold</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>Campmany</surname>
<given-names>E.</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>Dean</surname>
<given-names>S.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Ewen</surname>
<given-names>G. B. L.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff6">
<sup>6</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 contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Lawrence</surname>
<given-names>B. N.</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>Siddans</surname>
<given-names>R.</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>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>Watts</surname>
<given-names>P. D.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</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, \newline OX11 0QX, UK</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>EUMETSAT, Eumetsat-Allee 1, 64295 Darmstadt, Germany</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>now at: Earth Sciences Department, Barcelona Supercomputing Center, Jordi Girona 29, Barcelona 08034, Spain</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>now at: National Institute of Water and Atmospheric Research, Wellington, New Zealand</addr-line>
</aff>
<aff id="aff6">
<label>6</label>
<addr-line>now at: Credit Suisse, One Cabot Square, London E14 4QJ, UK</addr-line>
</aff>
<pub-date pub-type="epub">
<day>02</day>
<month>11</month>
<year>2010</year>
</pub-date>
<volume>10</volume>
<issue>11</issue>
<fpage>25619</fpage>
<lpage>25686</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-discuss.net/10/25619/2010/acpd-10-25619-2010.html">This article is available from http://www.atmos-chem-phys-discuss.net/10/25619/2010/acpd-10-25619-2010.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys-discuss.net/10/25619/2010/acpd-10-25619-2010.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys-discuss.net/10/25619/2010/acpd-10-25619-2010.pdf</self-uri>
<abstract>
<p>The Along-Track Scanning Radiometers (ATSRs) provide a long
      time-series of measurements suitable for the retrieval of cloud
      properties. This work evaluates the freely-available Global Retrieval
      of ATSR Cloud Parameters and Evaluation (GRAPE) dataset (version 3)
      created from the ATSR-2 (1995–2003) and Advanced ATSR (AATSR; 2002
      onwards) records. Users are recommended to consider only retrievals
      flagged as high-quality, where there is a good consistency between the
      measurements and the retrieved state (corresponding to about 60% of
      converged retrievals over sea, and more than 80% over land). Cloud
      properties are found to be generally free of any significant spurious
      trends relating to satellite zenith angle. Estimates of the random
      error on retrieved cloud properties are suggested to be generally
      appropriate for optically-thick clouds, and up to a factor of two too
      small for optically-thin cases. The correspondence between ATSR-2 and
      AATSR cloud properties is high, but a relative calibration difference
      between the sensors of order 5–10% at 660 nm and 870 nm limits
      the potential of the current version of the dataset for trend
      analysis. As ATSR-2 is thought to have the better absolute
      calibration, the discussion focusses on this portion of the
      record. Cloud-top heights from GRAPE compare well to ground-based data
      at four sites, particularly for shallow clouds. Clouds forming in
      boundary-layer inversions are typically around 1 km too high in GRAPE
      due to poorly-resolved inversions in the modelled temperature profiles
      used. Global cloud fields are compared to satellite products derived
      from the Moderate Resolution Imaging Spectroradiometer (MODIS),
      Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP)
      measurements, and a climatology of liquid water content derived from
      satellite microwave radiometers. In all cases the main reasons for
      differences are linked to differing sensitivity to, and treatment of,
      multi-layer cloud systems. The correlation coefficient between GRAPE
      and the two MODIS products considered is generally high (greater than
      0.7 for most cloud properties), except for liquid and ice cloud
      effective radius, which also show biases between the datasets. For
      liquid clouds, part of the difference is linked to choice of
      wavelengths used in the retrieval. Total cloud cover is slightly lower
      in GRAPE (0.64) than the CALIOP dataset (0.66). GRAPE underestimates
      liquid cloud water path relative to microwave radiometers by up to
      100 g m&lt;sup&gt;−2&lt;/sup&gt; near the Equator and overestimates by around
      50 g m&lt;sup&gt;−2&lt;/sup&gt; in the storm tracks. Finally, potential future
      improvements to the algorithm are outlined.</p>
</abstract>
<counts><page-count count="68"/></counts>
</article-meta>
</front>
<body/>
<back>
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