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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-8-17467-2008</article-id>
<title-group>
<article-title>Ozone Monitoring Instrument spectral UV irradiance products: comparison with ground based measurements at an urban environment</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Kazadzis</surname>
<given-names>S.</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>Bais</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>Arola</surname>
<given-names>A.</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>Krotkov</surname>
<given-names>N.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Kouremeti</surname>
<given-names>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>Meleti</surname>
<given-names>C.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Finnish Meteorological Institute, Research and Development, Helsinki, Finland</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Laboratory of Atmospheric Physics, Aristotle University Thessaloniki, Thessaloniki, Greece</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Finnish Meteorological Institute, Research and Development, Kuopio, Finland</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Goddard Earth Sciences and Technology Center, University of Maryland, Baltimore County, Baltimore, MD, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>24</day>
<month>09</month>
<year>2008</year>
</pub-date>
<volume>8</volume>
<issue>5</issue>
<fpage>17467</fpage>
<lpage>17493</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/8/17467/2008/acpd-8-17467-2008.html">This article is available from http://www.atmos-chem-phys-discuss.net/8/17467/2008/acpd-8-17467-2008.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys-discuss.net/8/17467/2008/acpd-8-17467-2008.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys-discuss.net/8/17467/2008/acpd-8-17467-2008.pdf</self-uri>
<abstract>
<p>We have compared spectral ultraviolet overpass irradiances from the Ozone
Monitoring Instruments (OMI) against ground-based Brewer measurements at
Thessaloniki, Greece from September 2004 to December 2007. It is
demonstrated that OMI overestimates UV irradiances by 30%, 17% and
13% for 305 nm, 324 nm, and 380 nm respectively and 20% for erythemally
weighted irradiance. The bias between OMI and Brewer increases with
increasing aerosol absorption optical thickness. We present methodologies
that can be applied for correcting this bias based on experimental results
derived from the comparison period and also theoretical approaches using
radiative transfer model calculations. All correction approaches minimize
the bias and the standard deviation of the ratio OMI versus Brewer ratio.
According to the results, the best correction approach suggests that the OMI
UV product has to be multiplied by a correction factor C&lt;sub&gt;&lt;i&gt;A&lt;/i&gt;&lt;/sub&gt;(λ)
are in the order of 0.8, 0.88 and 0.9 for 305 nm, 324 nm and 380 nm
respectively. Limitations and possibilities for applying such methodologies
in a global scale are also discussed.</p>
</abstract>
<counts><page-count count="27"/></counts>
</article-meta>
</front>
<body/>
<back>
<ref-list>
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</back>
</article>