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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-7-2881-2007</article-id>
<title-group>
<article-title>Technical Note: The effect of sensor resolution on the number of cloud-free observations from space</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Krijger</surname>
<given-names>J. 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>van Weele</surname>
<given-names>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>Aben</surname>
<given-names>I.</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>Frey</surname>
<given-names>R.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>SRON, Netherlands Institute for Space Research, Sorbonnelaan 2, 3584 CA Utrecht, The Netherlands</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>KNMI, Royal Netherlands Meteorological Institute, De Bilt, The Netherlands</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Cooperative Institute for Meteorological Satellite Studies, University of Wisconsin-Madison, Madison, WI, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>11</day>
<month>06</month>
<year>2007</year>
</pub-date>
<volume>7</volume>
<issue>11</issue>
<fpage>2881</fpage>
<lpage>2891</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/7/2881/2007/acp-7-2881-2007.html">This article is available from http://www.atmos-chem-phys.net/7/2881/2007/acp-7-2881-2007.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/7/2881/2007/acp-7-2881-2007.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/7/2881/2007/acp-7-2881-2007.pdf</self-uri>
<abstract>
<p>Air quality and surface emission inversions are likely to be focal points for future satellite
missions on atmospheric composition. Most important for these applications is sensitivity to
the atmospheric composition in the lowest few kilometers of the troposphere. Reduced sensitivity
by clouds needs to be minimized. In this study we have quantified the increase in number
of useful footprints, i.e. footprints which are sufficient cloud-free, as a function of sensor resolution (footprint area). 
High resolution
(1 km&amp;times;1 km) MODIS TERRA cloud mask observations are aggregated to lower resolutions. Statistics for
different thresholds on cloudiness are applied. For each month in 2004 four days of MODIS data are analyzed.
Globally the fraction of cloud-free observations  drops from 16% at 100 km&lt;sup&gt;2&lt;/sup&gt; resolution to only 3% at 
10 000 km&lt;sup&gt;2&lt;/sup&gt; if not
a single MODIS observation within a footprint is allowed to be cloudy. If up to 5% or 20% of a
footprint is allowed to be cloudy, the fraction of cloud-free observations  is 9% or 17%,  respectively, at
10 000 km&lt;sup&gt;2&lt;/sup&gt; resolution. The probability of finding cloud-free observations for different sensor
resolutions is also quantified as a function of geolocation and season, showing examples over
Europe and northern South America (ITCZ).</p>
</abstract>
<counts><page-count count="11"/></counts>
</article-meta>
</front>
<body/>
<back>
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</article>