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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-12-6723-2012</article-id>
<title-group>
<article-title>Tropospheric bromine chemistry: implications for present and pre-industrial ozone and mercury</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Parrella</surname>
<given-names>J. P.</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>Jacob</surname>
<given-names>D. 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>Liang</surname>
<given-names>Q.</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>Zhang</surname>
<given-names>Y.</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>Mickley</surname>
<given-names>L. 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>Miller</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>Evans</surname>
<given-names>M. J.</given-names>
</name>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
<xref ref-type="aff" rid="aff6">
<sup>6</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="aff7">
<sup>7</sup>
</xref>
<xref ref-type="aff" rid="aff8">
<sup>8</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Pyle</surname>
<given-names>J. A.</given-names>
</name>
<xref ref-type="aff" rid="aff7">
<sup>7</sup>
</xref>
<xref ref-type="aff" rid="aff8">
<sup>8</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Theys</surname>
<given-names>N.</given-names>
</name>
<xref ref-type="aff" rid="aff9">
<sup>9</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Van Roozendael</surname>
<given-names>M.</given-names>
</name>
<xref ref-type="aff" rid="aff9">
<sup>9</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>School of Engineering and Applied Sciences, Harvard University, Cambridge, MA, USA</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Universities Space Research Association GESTAR, Columbia, MD, USA</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>NASA Goddard Space Flight Center, Greenbelt, MD, USA</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Department of Atmospheric Sciences, University of Washington, Seattle, Washington, USA</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>Department of Chemistry, University of York, York, UK</addr-line>
</aff>
<aff id="aff6">
<label>6</label>
<addr-line>National Centre for Atmospheric Sciences (NCAS), York, UK</addr-line>
</aff>
<aff id="aff7">
<label>7</label>
<addr-line>National Centre for Atmospheric Sciences (NCAS), Cambridge, UK</addr-line>
</aff>
<aff id="aff8">
<label>8</label>
<addr-line>Centre for Atmospheric Sciences, Department of Chemistry, University of Cambridge, Cambridge, CB2 1EW, UK</addr-line>
</aff>
<aff id="aff9">
<label>9</label>
<addr-line>Belgian Institute for Space Aeronomy (IASB-BIRA), Brussels, Belgium</addr-line>
</aff>
<pub-date pub-type="epub">
<day>01</day>
<month>08</month>
<year>2012</year>
</pub-date>
<volume>12</volume>
<issue>15</issue>
<fpage>6723</fpage>
<lpage>6740</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/12/6723/2012/acp-12-6723-2012.html">This article is available from http://www.atmos-chem-phys.net/12/6723/2012/acp-12-6723-2012.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/12/6723/2012/acp-12-6723-2012.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/12/6723/2012/acp-12-6723-2012.pdf</self-uri>
<abstract>
<p>We present a new model for the global tropospheric chemistry of inorganic
bromine (Br&lt;sub&gt;y&lt;/sub&gt;) coupled to oxidant-aerosol chemistry in the GEOS-Chem
chemical transport model (CTM). Sources of tropospheric Br&lt;sub&gt;y&lt;/sub&gt; include
debromination of sea-salt aerosol, photolysis and oxidation of short-lived
bromocarbons, and transport from the stratosphere. Comparison to a GOME-2
satellite climatology of tropospheric BrO columns shows that the model can
reproduce the observed increase of BrO with latitude, the northern
mid-latitudes maximum in winter, and the Arctic maximum in spring. This
successful simulation is contingent on the HOBr + HBr reaction taking place in
aqueous aerosols and ice clouds. Bromine chemistry in the model decreases
tropospheric ozone mixing ratios by &lt;1–8 nmol mol&lt;sup&gt;−1&lt;/sup&gt; (6.5%
globally), with the largest effects in the northern extratropics in spring.
The global mean tropospheric OH concentration decreases by 4%. Inclusion
of bromine chemistry improves the ability of global models (GEOS-Chem and
p-TOMCAT) to simulate observed 19th-century ozone and its seasonality.
Bromine effects on tropospheric ozone are comparable in the present-day and
pre-industrial atmospheres so that estimates of anthropogenic radiative
forcing are minimally affected. Br atom concentrations are 40% higher in
the pre-industrial atmosphere due to lower ozone, which would decrease by a
factor of 2 the atmospheric lifetime of elemental mercury against oxidation
by Br. This suggests that historical anthropogenic mercury emissions may
have mostly deposited to northern mid-latitudes, enriching the corresponding
surface reservoirs. The persistent rise in background surface ozone at
northern mid-latitudes during the past decades could possibly contribute to
the observations of elevated mercury in subsurface waters of the North
Atlantic.</p>
</abstract>
<counts><page-count count="18"/></counts>
</article-meta>
</front>
<body/>
<back>
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