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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-11-4689-2011</article-id>
<title-group>
<article-title>The 2009 stratospheric major warming described from synergistic use of BASCOE water vapour analyses and MLS observations</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Lahoz</surname>
<given-names>W. A.</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 contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Errera</surname>
<given-names>Q.</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>Viscardy</surname>
<given-names>S.</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>Manney</surname>
<given-names>G. L.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Norsk Institutt for Luftforskning, NILU, Norway</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>CNRM-GAME, URA1357, Météo-France and CNRS, Toulouse, France</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Institut d&apos;Aéronomie Spatiale de Belgique, BIRA-IASB, Belgium</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA, USA</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>New Mexico Institute of Mining and Technology, NM, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>20</day>
<month>05</month>
<year>2011</year>
</pub-date>
<volume>11</volume>
<issue>10</issue>
<fpage>4689</fpage>
<lpage>4703</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/11/4689/2011/acp-11-4689-2011.html">This article is available from http://www.atmos-chem-phys.net/11/4689/2011/acp-11-4689-2011.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/11/4689/2011/acp-11-4689-2011.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/11/4689/2011/acp-11-4689-2011.pdf</self-uri>
<abstract>
<p>The record-breaking major stratospheric warming of northern winter 2009
(January–February) is studied using BASCOE (Belgian Assimilation System for
Chemical ObsErvation) stratospheric water vapour analyses and MLS (Microwave
Limb Sounder) water vapour observations, together with meteorological data
from the European Centre for Medium-Range Weather Forecasts (ECMWF) and
potential vorticity (PV) derived from ECMWF meteorological data. We focus on
the interaction between the cyclonic wintertime stratospheric polar vortex
and subsidiary anticyclonic stratospheric circulations during the build-up,
peak and aftermath of the major warming. We show dynamical consistency
between the water vapour analysed fields and the meteorological and PV
fields. Using various approaches, we use the analysed water vapour fields to
estimate descent in the polar vortex during this period of between
~0.5 km day&lt;sup&gt;−1&lt;/sup&gt; and ~0.7 km day&lt;sup&gt;−1&lt;/sup&gt;. New results include the
analysis of water vapour during the major warming and demonstration of the
benefit of assimilating MLS satellite data into the BASCOE model.</p>
</abstract>
<counts><page-count count="15"/></counts>
</article-meta>
</front>
<body/>
<back>
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