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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-12-9881-2012</article-id>
<title-group>
<article-title>Aircraft measurements of wave clouds</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Cui</surname>
<given-names>Z.</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>Blyth</surname>
<given-names>A. M.</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>Bower</surname>
<given-names>K. N.</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>Crosier</surname>
<given-names>J.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Choularton</surname>
<given-names>T.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Institute for Climate and Atmospheric Science, School of Earth and Environment, University of Leeds, UK</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>National Centre for Atmospheric Science, UK</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Centre for Atmospheric Science, SEAES, University of Manchester, UK</addr-line>
</aff>
<pub-date pub-type="epub">
<day>29</day>
<month>10</month>
<year>2012</year>
</pub-date>
<volume>12</volume>
<issue>20</issue>
<fpage>9881</fpage>
<lpage>9892</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/12/9881/2012/acp-12-9881-2012.html">This article is available from http://www.atmos-chem-phys.net/12/9881/2012/acp-12-9881-2012.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/12/9881/2012/acp-12-9881-2012.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/12/9881/2012/acp-12-9881-2012.pdf</self-uri>
<abstract>
<p>In this paper, aircraft measurements are presented of liquid phase
(ice-free) wave clouds made at temperatures greater than −5&amp;deg;C
that formed over Scotland, UK. The horizontal variations
of the vertical velocity across wave clouds display a distinct pattern.
The maximum updraughts occur at the upshear flanks of the clouds and
the strong downdraughts at the downshear flanks. The cloud droplet
concentrations were a couple of hundreds per cubic centimetres,
and the drops generally had a mean diameter between 15–45 μm.
A small proportion of the drops were drizzle. The measurements presented
 here and in previous recent studies suggest a different interaction
of dynamics and microphysics in wave clouds from the accepted model.
The results in this paper provide a case for future numerical
simulation of wave cloud and the interaction between wave and cloud.</p>
</abstract>
<counts><page-count count="12"/></counts>
</article-meta>
</front>
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