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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>GÃ¶ttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acpd-8-2849-2008</article-id>
<title-group>
<article-title>Correlation between equatorial Kelvin waves and the occurrence of extremely thin ice clouds at the tropical tropopause</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Immler</surname>
<given-names>F.</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>KrÃ¼ger</surname>
<given-names>K.</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>Fujiwara</surname>
<given-names>M.</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>Verver</surname>
<given-names>G.</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>Rex</surname>
<given-names>M.</given-names>
</name>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Schrems</surname>
<given-names>O.</given-names>
</name>
<xref ref-type="aff" rid="aff6">
<sup>6</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>German Meteorological Service, Richard-AÃŸmann-Observatory, Lindenberg, Germany</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>IFM-GEOMAR, Kiel, Germany</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Hokkaido University, Faculty of Environmental Earth Science, Japan</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Royal Netherlands Meteorological Institute (KNMI), De Bilt, The Netherlands</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>Alfred Wegener Institute for Polar and Marine Research, Potsdam, Germany</addr-line>
</aff>
<aff id="aff6">
<label>6</label>
<addr-line>Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany</addr-line>
</aff>
<pub-date pub-type="epub">
<day>13</day>
<month>02</month>
<year>2008</year>
</pub-date>
<volume>8</volume>
<issue>1</issue>
<fpage>2849</fpage>
<lpage>2862</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/8/2849/2008/acpd-8-2849-2008.html">This article is available from http://www.atmos-chem-phys-discuss.net/8/2849/2008/acpd-8-2849-2008.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys-discuss.net/8/2849/2008/acpd-8-2849-2008.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys-discuss.net/8/2849/2008/acpd-8-2849-2008.pdf</self-uri>
<abstract>
<p>A number of field-campaigns in the tropics have been conducted in
the recent years with two different LIDAR systems at Paramaribo in
Suriname (5.8&amp;deg; N, 55.2&amp;deg; W). The lidars detect particles
in the atmosphere with high vertical and temporal resolution and are
capable of detecting extremely thin cloud layers which frequently occur
in the tropical tropopause layer (TTL). Radiosonde as well as operational
ECMWF analysis show that temperature anomalies caused by equatorial Kelvin
waves propagate downward, well below the cold point tropopause (CPT). We
find a clear correlation between the temperature anomalies introduced by
these waves and the occurrence of thin cirrus in the TTL. In particular
we found that extremely thin ice clouds form regularly where cold anomalies
shift the tropopause to high altitudes. This finding suggests an influence of
Kelvin wave activity on the dehydration in the TTL and thus on the global
stratospheric water vapour concentration.</p>
</abstract>
<counts><page-count count="14"/></counts>
</article-meta>
</front>
<body/>
<back>
<ref-list>
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</back>
</article>