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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ACPD</journal-id>
<journal-title-group>
<journal-title>Atmospheric Chemistry and Physics Discussions</journal-title>
<abbrev-journal-title abbrev-type="publisher">ACPD</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7375</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/acpd-12-4477-2012</article-id>
<title-group>
<article-title>Bridging the gap between bromocarbon oceanic emissions and upper air concentrations</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Tegtmeier</surname>
<given-names>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>Krüger</surname>
<given-names>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>Quack</surname>
<given-names>B.</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>Pisso</surname>
<given-names>I.</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>Stohl</surname>
<given-names>A.</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>Yang</surname>
<given-names>X.</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>IFM-GEOMAR, Kiel, Germany</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Research Institute for Global Change, JAMSTEC, Yokohama, Japan</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Norwegian Institute for Air Research (NILU), Kjeller, Norway</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>National Centre for Atmospheric Science (NCAS), Cambridge, UK</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>University of Cambridge, Department of Chemistry, Cambridge, UK</addr-line>
</aff>
<pub-date pub-type="epub">
<day>08</day>
<month>02</month>
<year>2012</year>
</pub-date>
<volume>12</volume>
<issue>2</issue>
<fpage>4477</fpage>
<lpage>4505</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-discuss.net/12/4477/2012/acpd-12-4477-2012.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys-discuss.net/12/4477/2012/acpd-12-4477-2012.pdf</self-uri>
<abstract>
<p>Oceanic emissions of halogenated very short-lived substances (VSLS) are
expected to contribute significantly to the stratospheric halogen loading
and therefore to ozone depletion. Estimates of the amount of VSLS
transported into the stratosphere are highly uncertain and based on sporadic
observations around the tropical tropopause layer (TTL) and on modeling
studies which use prescribed emission scenarios to reproduce observed
atmospheric concentrations. Actual measurements of VSLS emissions at the
ocean surface have not been linked to the stratospheric halogen loading
until now. Here we use observations of oceanic VSLS emissions in the western
Pacific and an atmospheric Lagrangian transport model to estimate the direct
contribution of bromoform (CHBr&lt;sub&gt;3&lt;/sub&gt;), and dibromomethane
(CH&lt;sub&gt;2&lt;/sub&gt;Br&lt;sub&gt;2&lt;/sub&gt;) to the stratospheric bromine loading. Our
emission-based estimates of VSLS profiles provide the first link between
observed oceanic emissions and in situ TTL measurements. The emission-based
and observed profiles of CHBr&lt;sub&gt;3&lt;/sub&gt; show good agreement, confirming the
importance of the western Pacific as a source region. However, CH&lt;sub&gt;2&lt;/sub&gt;Br&lt;sub&gt;2&lt;/sub&gt;
emission-based estimates are considerable smaller than current
upper air observations as a result of relatively low western Pacific
emissions. We estimate the relative importance of the highly variable
emission rates and the surface to stratosphere transport for the
contribution of the two bromocarbons to the stratospheric bromine budget.
Our results show that stratospheric entrainment of bromine in form of VSLS
or their degradation products is highly variable and that this variability
is primarily linked to the variability of the observed sea-to-air flux.
Together, both bromocarbons contribute to the stratospheric bromine budget
with 0.4 pptv on average and 2.3 pptv for cases of maximum emissions.</p>
</abstract>
<counts><page-count count="29"/></counts>
</article-meta>
</front>
<body/>
<back>
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