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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>
</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-11-5485-2011</article-id>
<title-group>
<article-title>Tropopause height at 78&amp;deg; N 16&amp;deg; E: average seasonal variation 2007–2010</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Hall</surname>
<given-names>C. 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>Hansen</surname>
<given-names>G.</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>Sigernes</surname>
<given-names>F.</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>Kuyeng Ruiz</surname>
<given-names>K. M.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Tromsø Geophysical Observatory, University of Tromsø, Norway</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Norwegian Institute for Air Research, Tromsø, Norway</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>The University Centre in Svalbard, Longyearbyen, Norway</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Jicamarca Radio Observatory, Lima, Peru</addr-line>
</aff>
<pub-date pub-type="epub">
<day>15</day>
<month>06</month>
<year>2011</year>
</pub-date>
<volume>11</volume>
<issue>11</issue>
<fpage>5485</fpage>
<lpage>5490</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/11/5485/2011/acp-11-5485-2011.html">This article is available from http://www.atmos-chem-phys.net/11/5485/2011/acp-11-5485-2011.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/11/5485/2011/acp-11-5485-2011.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/11/5485/2011/acp-11-5485-2011.pdf</self-uri>
<abstract>
<p>We present a seasonal climatology of tropopause altitude for 78° N 16° E
derived from observations 2007–2010 by the SOUSY VHF radar on Svalbard.
The spring minimum occurs one month later than that of surface air
temperature and instead coincides with the maximum in ozone column density.
This confirms similar studies based on radiosonde measurements in the arctic
and demonstrates downward control by the stratosphere. If one is to exploit
the potential of tropopause height as a metric for climate change at high
latitude and elsewhere, it is imperative to observe and understand the
processes which establish the tropopause – an understanding to which this
study contributes.</p>
</abstract>
<counts><page-count count="6"/></counts>
</article-meta>
</front>
<body/>
<back>
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</article>