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<front>
<journal-meta>
<journal-id journal-id-type="publisher">AMT</journal-id>
<journal-title-group>
<journal-title>Atmospheric Measurement Techniques</journal-title>
<abbrev-journal-title abbrev-type="publisher">AMT</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Atmos. Meas. Tech.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1867-8548</issn>
<publisher><publisher-name>Copernicus Publications</publisher-name>
<publisher-loc>GÃ¶ttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/amt-4-131-2011</article-id>
<title-group>
<article-title>Intercomparison of column aerosol optical depths from CALIPSO and MODIS-Aqua</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Kittaka</surname>
<given-names>C.</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>Winker</surname>
<given-names>D. M.</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>Vaughan</surname>
<given-names>M. 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>Omar</surname>
<given-names>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>Remer</surname>
<given-names>L. 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>Science Systems and Applications Inc., Hampton, VA, USA</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>NASA Langley Research Center, Hampton, VA, USA</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>NASA Goddard Spaceflight Center, Greenbelt, MD, USA</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>deceased</addr-line>
</aff>
<pub-date pub-type="epub">
<day>01</day>
<month>02</month>
<year>2011</year>
</pub-date>
<volume>4</volume>
<issue>2</issue>
<fpage>131</fpage>
<lpage>141</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2011 C. Kittaka et al.</copyright-statement>
<copyright-year>2011</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://amt.copernicus.org/articles/4/131/2011/amt-4-131-2011.html">This article is available from https://amt.copernicus.org/articles/4/131/2011/amt-4-131-2011.html</self-uri>
<self-uri xlink:href="https://amt.copernicus.org/articles/4/131/2011/amt-4-131-2011.pdf">The full text article is available as a PDF file from https://amt.copernicus.org/articles/4/131/2011/amt-4-131-2011.pdf</self-uri>
<abstract>
<p>The Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) is carried on
the CALIPSO satellite and has acquired global aerosol profiles since June
2006. CALIPSO is flown in formation with the Aqua satellite as part of the
A-train satellite constellation, so that a large number of coincident
aerosol observations are available from CALIOP and the MODIS-Aqua
instrument. This study compares column aerosol optical depth at 0.532  Î¼m
derived from CALIOP aerosol profiles with MODIS-Aqua 0.55 Î¼m aerosol
optical depth over the period June 2006 through August 2008. The study is
based on the CALIOP Version 2 Aerosol Layer Product and MODIS Collection 5.
While CALIOP is first and foremost a profiling instrument, this comparison
of column aerosol optical depth provides insight into quality of CALIOP
aerosol data. It is found that daytime aerosol optical depth from the CALIOP
Version 2 product has only a small global mean bias relative to MODIS
Collection 5. Regional biases, of both signs, are larger and biases are seen
to vary somewhat with season. Good agreement between the two sensors in ocean regions with low
cloudiness suggests that the selection of lidar ratios used in the
CALIOP aerosol retrieval is sufficient to provide a regional mean AOD
consistent with that retrieved from MODIS. Although differences over land are observed to
be larger than over ocean, the bias between CALIOP and MODIS AOD on a
regional-seasonal basis is found to be roughly within the envelope of the
MODIS expected uncertainty over land and ocean. This work forms a basis for
further comparisons using the recently released CALIOP Version 3 data.</p>
</abstract>
<counts><page-count count="11"/></counts>
</article-meta>
</front>
<body/>
<back>
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</article>