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<article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" article-type="research-article" dtd-version="3.0" xml:lang="en">
<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-5-1589-2005</article-id>
<title-group>
<article-title>Solar occultation with SCIAMACHY: algorithm description and first validation</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Meyer</surname>
<given-names>J.</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>Bracher</surname>
<given-names>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>Rozanov</surname>
<given-names>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>Schlesier</surname>
<given-names>A. 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>Bovensmann</surname>
<given-names>H.</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-group><aff id="aff1">
<label>1</label>
<addr-line>Institute of Environmental Physics, University of Bremen, Germany</addr-line>
</aff>
<pub-date pub-type="epub">
<day>22</day>
<month>06</month>
<year>2005</year>
</pub-date>
<volume>5</volume>
<issue>6</issue>
<fpage>1589</fpage>
<lpage>1604</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/5/1589/2005/acp-5-1589-2005.html">This article is available from http://www.atmos-chem-phys.net/5/1589/2005/acp-5-1589-2005.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/5/1589/2005/acp-5-1589-2005.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/5/1589/2005/acp-5-1589-2005.pdf</self-uri>
<abstract>
<p>This presentation concentrates on solar occultation measurements with the
spaceborne spectrometer SCIAMACHY in the UV-Vis wavelength range. Solar
occultation measurements provide unique information about the vertical
distribution of atmospheric constituents. For retrieval of vertical trace gas
concentration profiles, an algorithm has been developed based on the optimal
estimation method. The forward model is capable of simulating the extinction
signals of different species as they occur in atmospheric transmission
spectra obtained from occultation measurements. Furthermore, correction
algorithms have been implemented to address shortcomings of the tangent
height pre-processing and inhomogeneities of measured solar spectra. First
results of O&lt;sub&gt;3&lt;/sub&gt; and NO&lt;sub&gt;2&lt;/sub&gt; vertical profile retrievals have been validated
with data from ozone sondes and satellite based occultation instruments. The
validation shows very promising results for SCIAMACHY O&lt;sub&gt;3&lt;/sub&gt; and NO&lt;sub&gt;2&lt;/sub&gt; values
between 15 to 35km with errors of the order of 10% and 15%,
respectively.</p>
</abstract>
<counts><page-count count="16"/></counts>
</article-meta>
</front>
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