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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>
<abbrev-journal-title abbrev-type="nlm-ta">Atmos. Chem. Phys.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7324</issn>
<publisher><publisher-name>Copernicus Publications</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acp-9-4639-2009</article-id>
<title-group>
<article-title>BrO, blizzards, and drivers of polar tropospheric ozone depletion events</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Jones</surname>
<given-names>A. E.</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>Anderson</surname>
<given-names>P. S.</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>Begoin</surname>
<given-names>M.</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>Brough</surname>
<given-names>N.</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>Hutterli</surname>
<given-names>M. 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>Marshall</surname>
<given-names>G. J.</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>Richter</surname>
<given-names>A.</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>Roscoe</surname>
<given-names>H. K.</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>Wolff</surname>
<given-names>E. W.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>British Antarctic Survey, Natural Environment Research Council, High Cross, Madingley Road, Cambridge, CB3 0ET, UK</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Institute of Environmental Physics, University of Bremen, Otto-Hahn-Allee 1, 28359 Bremen, Germany</addr-line>
</aff>
<pub-date pub-type="epub">
<day>17</day>
<month>07</month>
<year>2009</year>
</pub-date>
<volume>9</volume>
<issue>14</issue>
<fpage>4639</fpage>
<lpage>4652</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2009 A. E. Jones et al.</copyright-statement>
<copyright-year>2009</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 3.0 Unported License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by/3.0/">https://creativecommons.org/licenses/by/3.0/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://acp.copernicus.org/articles/9/4639/2009/acp-9-4639-2009.html">This article is available from https://acp.copernicus.org/articles/9/4639/2009/acp-9-4639-2009.html</self-uri>
<self-uri xlink:href="https://acp.copernicus.org/articles/9/4639/2009/acp-9-4639-2009.pdf">The full text article is available as a PDF file from https://acp.copernicus.org/articles/9/4639/2009/acp-9-4639-2009.pdf</self-uri>
<abstract>
<p>The source of bromine that drives polar boundary
layer ozone depletion events (ODEs) is still open to some debate. While ODEs
are generally noted to form under conditions of a shallow stable boundary
layer, observations of depleted air under high wind conditions are taken as
being transport-related. Here we report observations from Antarctica in
which an unusually large cloud of BrO formed over the Weddell Sea. The
enhanced BrO was observed over Halley station in coastal Antarctica,
providing an opportunity to probe the conditions within an active &quot;bromine
explosion&quot; event. On this occasion, enhanced BrO and depleted boundary
layer ozone coincided with high wind speeds and saline blowing snow. We
derive a simple model to consider the environmental conditions that favour
ODEs and find two maxima, one at low wind/stable boundary layer and one at
high wind speeds with blowing snow. Modelling calculations aiming to
reproduce the wider regional or global impacts of ODEs, either via radiative
effects or as a halogen source, will also need to account for high wind
speed mechanisms.</p>
</abstract>
<counts><page-count count="14"/></counts>
</article-meta>
</front>
<body/>
<back>
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