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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-7-4171-2007</article-id>
<title-group>
<article-title>Observations of OH and HO&lt;sub&gt;2&lt;/sub&gt; radicals in coastal Antarctica</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Bloss</surname>
<given-names>W. J.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</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>Lee</surname>
<given-names>J. D.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Heard</surname>
<given-names>D. 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>Salmon</surname>
<given-names>R. 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>Bauguitte</surname>
<given-names>S. J.-B.</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="aff2">
<sup>2</sup>
</xref>
</contrib>
<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="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>School of Chemistry, University of Leeds, Woodhouse Lane, Leeds, LS2 9JT, UK</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>British Antarctic Survey, Madingley Road, Cambridge, CB3 0ET, UK</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>now at: School of Geography, Earth &amp; Environmental Sciences, University of Birmingham, Edgbaston, Birmingham, B15 2TT, UK</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>now at: Department of Chemistry, University of York, Heslington, York, YO10 5DD, UK</addr-line>
</aff>
<pub-date pub-type="epub">
<day>16</day>
<month>08</month>
<year>2007</year>
</pub-date>
<volume>7</volume>
<issue>16</issue>
<fpage>4171</fpage>
<lpage>4185</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2007 W. J. Bloss et al.</copyright-statement>
<copyright-year>2007</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 Generic License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by-nc-sa/2.5/">https://creativecommons.org/licenses/by-nc-sa/2.5/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://acp.copernicus.org/articles/7/4171/2007/acp-7-4171-2007.html">This article is available from https://acp.copernicus.org/articles/7/4171/2007/acp-7-4171-2007.html</self-uri>
<self-uri xlink:href="https://acp.copernicus.org/articles/7/4171/2007/acp-7-4171-2007.pdf">The full text article is available as a PDF file from https://acp.copernicus.org/articles/7/4171/2007/acp-7-4171-2007.pdf</self-uri>
<abstract>
<p>OH and HO&lt;sub&gt;2&lt;/sub&gt; radical concentrations have been measured in the boundary
layer of coastal Antarctica for a six-week period during the austral summer
of 2005. The measurements were performed at the British Antarctic Survey&apos;s
Halley Research Station (75&amp;deg; 35&apos; S, 26&amp;deg; 19&apos; W), using the technique
of on-resonance laser-induced fluorescence to detect OH, with HO&lt;sub&gt;2&lt;/sub&gt;
measured following chemical conversion through addition of NO. The mean
radical levels were 3.9&amp;times;10&lt;sup&gt;5&lt;/sup&gt; molecule cm&lt;sup&gt;&amp;minus;3&lt;/sup&gt; for OH, and
0.76 ppt for HO&lt;sub&gt;2&lt;/sub&gt; (ppt denotes parts per trillion, by volume). Typical
maximum (local noontime) levels were 7.9&amp;times;10&lt;sup&gt;5&lt;/sup&gt; molecule cm&lt;sup&gt;&amp;minus;3&lt;/sup&gt;
and 1.50 ppt for OH and HO&lt;sub&gt;2&lt;/sub&gt; respectively. The main sources of HO&lt;sub&gt;x&lt;/sub&gt;
were photolysis of O&lt;sub&gt;3&lt;/sub&gt; and HCHO, with potentially important but
uncertain contributions from HONO and higher aldehydes. Of the measured OH
sinks, reaction with CO and CH&lt;sub&gt;4&lt;/sub&gt; dominated, however comparison of the
observed OH concentrations with those calculated via the steady state
approximation indicated that additional co-reactants were likely to have
been present. Elevated levels of NO&lt;sub&gt;x&lt;/sub&gt; resulting from snowpack
photochemistry contributed to HO&lt;sub&gt;x&lt;/sub&gt; cycling and enhanced levels of OH,
however the halogen oxides IO and BrO dominated the CH&lt;sub&gt;3&lt;/sub&gt;O&lt;sub&gt;2&lt;/sub&gt; &amp;ndash;
HO&lt;sub&gt;2&lt;/sub&gt; &amp;ndash; OH conversion in this environment, with associated ozone
destruction.</p>
</abstract>
<counts><page-count count="15"/></counts>
</article-meta>
</front>
<body/>
<back>
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