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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-8-7265-2008</article-id>
<title-group>
<article-title>Bromine in the tropical troposphere and stratosphere as derived from balloon-borne BrO observations</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Dorf</surname>
<given-names>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>Butz</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>Camy-Peyret</surname>
<given-names>C.</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>Chipperfield</surname>
<given-names>M. P.</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>Kritten</surname>
<given-names>L.</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>Pfeilsticker</surname>
<given-names>K.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Institut für Umweltphysik (IUP), University of Heidelberg, Heidelberg, Germany</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>SRON–Netherlands Institute for Space Research, Utrecht, The Netherlands</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Laboratoire de Physique Moléculaire pour l&apos;Atmosphère et  l&apos;Astrophysique (LPMAA), Université Pierre et Marie Curie, Paris, France</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Institute for Atmospheric Science, School of Earth and Environment, University of Leeds, Leeds, UK</addr-line>
</aff>
<pub-date pub-type="epub">
<day>10</day>
<month>12</month>
<year>2008</year>
</pub-date>
<volume>8</volume>
<issue>23</issue>
<fpage>7265</fpage>
<lpage>7271</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>
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<self-uri xlink:href="http://www.atmos-chem-phys.net/8/7265/2008/acp-8-7265-2008.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/8/7265/2008/acp-8-7265-2008.pdf</self-uri>
<abstract>
<p>The first tropospheric and stratospheric (4 to 33 km) BrO profile is
presented for the inner tropics derived from balloon-borne DOAS (Differential
Optical Absorption Spectroscopy) measurements. In combination with
photochemical modelling, total stratospheric inorganic bromine (Br&lt;sub&gt;y&lt;/sub&gt;)
is deduced to be (21.5&amp;plusmn;2.5) ppt in 4.5-year-old air, probed in 2005. We
derive a total contribution of (5.2&amp;plusmn;2.5) ppt from brominated very
short-lived substances and inorganic product gases to stratospheric
Br&lt;sub&gt;y&lt;/sub&gt; Tropospheric BrO was found to be &lt;1 ppt. Our results
are compared to two 3-D CTM SLIMCAT model runs, which differ in the lifetime
of the bromine source gases, affecting the vertical distribution of
Br&lt;sub&gt;y&lt;/sub&gt; in the lower stratosphere. Bromine source gas measurements
performed 10 days earlier Laube et al., 2008, indicate a lower Br&lt;sub&gt;y&lt;/sub&gt; of
(17.5&amp;plusmn;0.4) ppt. Potential reasons for this discrepancy are discussed.</p>
</abstract>
<counts><page-count count="7"/></counts>
</article-meta>
</front>
<body/>
<back>
<ref-list>
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