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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-6-673-2006</article-id>
<title-group>
<article-title>Validation of SCIAMACHY top-of-atmosphere reflectance for aerosol remote sensing using MERIS L1 data</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>von Hoyningen-Huene</surname>
<given-names>W.</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>Kokhanovsky</surname>
<given-names>A. A.</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>Wuttke</surname>
<given-names>M. W.</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>Buchwitz</surname>
<given-names>M.</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>Noël</surname>
<given-names>S.</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>Gerilowski</surname>
<given-names>K.</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>Burrows</surname>
<given-names>J. P.</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>Latter</surname>
<given-names>B.</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>Kerridge</surname>
<given-names>B. J.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Institute of Environmental Physics/Remote Sensing, University of Bremen, Germany</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Space Science and Technology Department, Rutherford Appleton Laboratories, Chilton, UK</addr-line>
</aff>
<pub-date pub-type="epub">
<day>18</day>
<month>01</month>
<year>2006</year>
</pub-date>
<volume>6</volume>
<issue>1</issue>
<fpage>673</fpage>
<lpage>699</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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<self-uri xlink:href="http://www.atmos-chem-phys-discuss.net/6/673/2006/acpd-6-673-2006.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys-discuss.net/6/673/2006/acpd-6-673-2006.pdf</self-uri>
<abstract>
<p>Aerosol remote sensing is very much dependent on the quite
accurate knowledge of the top-of-atmosphere (TOA) reflectance
retrieved by a particular instrument. The status of the
calibration of such an instrument thus is reflected in the quality
of the aerosol retrieval. Currently the SCIAMACHY (SCanning
Imaging Absorption spectroMeter for Atmospheric CHartographY)
instrument gives too low values of the TOA reflectance, compared
e.g. to data from MERIS (Medium Resolution Imaging Spectrometer),
both operating on ENVISAT (ENVIronmental SATellite), but the
calibration of the operational L1 product of SCIAMACHY is not yet
finished.
&lt;br&gt;&lt;br&gt;
From an inter-comparison of MERIS and SCIAMACHY TOA reflectance,
for collocated scenes correction factors are derived to improve
the current SCIAMACHY L1 data for the purpose of aerosol remote
sensing. The corrected reflectance has been used for a first
remote sensing of the aerosol optical thickness by the BAER
(Bremen AErosol Retrieval) approach using SCIAMACHY data.</p>
</abstract>
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