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<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>
<abbrev-journal-title abbrev-type="nlm-ta">Atmos. Chem. Phys.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7324</issn>
<publisher><publisher-name>Copernicus Publications</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acp-14-5599-2014</article-id>
<title-group>
<article-title>Impact of cirrus clouds heterogeneities on top-of-atmosphere thermal  infrared radiation</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Fauchez</surname>
<given-names>T.</given-names>
<ext-link>https://orcid.org/0000-0002-5967-9631</ext-link>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Cornet</surname>
<given-names>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>Szczap</surname>
<given-names>F</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>Dubuisson</surname>
<given-names>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>Rosambert</surname>
<given-names>T.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Laboratoire d&apos;Optique Atmosphérique, Université Lille 1, Villeneuve d&apos;Ascq, France</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Laboratoire de Météorologie Physique, Université Blaise Pascal, Clermont Ferrand, France</addr-line>
</aff>
<pub-date pub-type="epub">
<day>05</day>
<month>06</month>
<year>2014</year>
</pub-date>
<volume>14</volume>
<issue>11</issue>
<fpage>5599</fpage>
<lpage>5615</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2014 T. Fauchez et al.</copyright-statement>
<copyright-year>2014</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://acp.copernicus.org/articles/14/5599/2014/acp-14-5599-2014.html">This article is available from https://acp.copernicus.org/articles/14/5599/2014/acp-14-5599-2014.html</self-uri>
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<abstract>
<p>This paper presents a study of the impact of cirrus cloud heterogeneities on
the thermal infrared brightness temperatures at the top of the atmosphere (TOA).
Realistic 3-D cirri are generated by a cloud generator based on simplified
thermodynamic and dynamic equations and on the control of invariant scale
properties. The 3-D thermal infrared radiative transfer is simulated with a
Monte Carlo model for three typical spectral bands in the infrared
atmospheric window. Comparisons of TOA brightness temperatures resulting from
1-D and 3-D radiative transfer show significant differences for optically
thick cirrus (τ &gt; 0.3 at 532 nm) and are mainly due to the
plane-parallel approximation (PPA). At the spatial resolution of
1 km × 1 km, two principal parameters control the heterogeneity
effects on brightness temperatures: i) the optical thickness standard
deviation inside the observation pixel, ii) the brightness temperature
contrast between the top of the cirrus~and the clear-sky atmosphere.
Furthermore, we show that the difference between 1-D and 3-D brightness
temperatures increases with the zenith view angle from two to ten times
between 0° and 60° due to the tilted independent pixel
approximation (TIPA).</p>
</abstract>
<counts><page-count count="17"/></counts>
</article-meta>
</front>
<body/>
<back>
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