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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-7-12927-2007</article-id>
<title-group>
<article-title>Do supersonic aircraft avoid contrails?</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Stenke</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>Grewe</surname>
<given-names>V.</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>Pechtl</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-group><aff id="aff1">
<label>1</label>
<addr-line>Deutsches Zentrum für Luft- und Raumfahrt, Institut für Physik der Atmosphäre, Oberpfaffenhofen, 82230 Wessling, Germany</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>now at: German Patent Office, 80297 München, Germany</addr-line>
</aff>
<pub-date pub-type="epub">
<day>04</day>
<month>09</month>
<year>2007</year>
</pub-date>
<volume>7</volume>
<issue>5</issue>
<fpage>12927</fpage>
<lpage>12958</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/7/12927/2007/acpd-7-12927-2007.html">This article is available from http://www.atmos-chem-phys-discuss.net/7/12927/2007/acpd-7-12927-2007.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys-discuss.net/7/12927/2007/acpd-7-12927-2007.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys-discuss.net/7/12927/2007/acpd-7-12927-2007.pdf</self-uri>
<abstract>
<p>The impact of a potential future fleet of supersonic aircraft on
  contrail coverage and contrail radiative forcing is investigated by
  means of simulations with the general circulation model
  ECHAM4.L39(DLR) including a contrail parameterization. The model
  simulations consider air traffic inventories of a subsonic fleet and
  of a combined fleet of sub- and supersonic aircraft for the years
  2025 and 2050, respectively. In case of the combined fleet, part of
  the subsonic fleet is replaced by supersonic aircraft. Supersonic
  aircraft fly at higher cruise levels (18 to 20 km) than subsonic
  aircraft (10 to 12 km). The different ambient meteorological
  conditions in terms of temperature and humidity affect the formation
  of contrails. At subsonic cruise levels, the combined air traffic
  scenario reveals a reduction in contrail cover in northern
  extratropics, especially over the North Atlantic and Pacific. At
  supersonic flight levels, contrail formation is mainly restricted to
  tropical regions. The northern extratropical stratosphere is only in
  winter cold enough for the formation of contrails. Total contrail
  coverage is only marginally affected by the shift in flight
  altitude. The model simulations indicate a global annual mean
  contrail cover of 0.372% for the subsonic and 0.366% for the
  combined fleet in 2050, respectively. The simulated contrail
  radiative forcing is most closely correlated to the total contrail
  cover, although contrails in the tropical lower stratosphere are
  found to be optically thinner than contrails in the extratropical
  upper troposphere. The global annual mean contrail radiative forcing
  in 2050 (2025) amounts to 24.7 mW m&lt;sup&gt;&amp;minus;2&lt;/sup&gt; (9.4 mW m&lt;sup&gt;&amp;minus;2&lt;/sup&gt;) for
  the subsonic fleet and 24.2 mW m&lt;sup&gt;&amp;minus;2&lt;/sup&gt; (9.3 mW m&lt;sup&gt;&amp;minus;2&lt;/sup&gt;) for
  the combined fleet. A reduced supersonic cruise speed (Mach 1.6
  instead of Mach 2.0) leads to a downward shift in contrail cover,
  but does not affect global mean total contrail cover and contrail radiative
  forcing. Hence the partial substitution of subsonic air traffic
  leads to a shift of contrail occurrence from mid to low latitudes,
  but the resulting change in contrail-induced climate impact is
  almost negligible.</p>
</abstract>
<counts><page-count count="32"/></counts>
</article-meta>
</front>
<body/>
<back>
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