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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-7-4661-2007</article-id>
<title-group>
<article-title>Tropospheric OH and Cl levels deduced from non-methane hydrocarbon measurements in a marine site</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Arsene</surname>
<given-names>C.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Bougiatioti</surname>
<given-names>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>Kanakidou</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>Bonsang</surname>
<given-names>B.</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>Mihalopoulos</surname>
<given-names>N.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Environmental Chemical Processes Laboratory, Department of Chemistry, University of Crete, 71003 Heraklion, Greece</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Inorganic and Analytical Chemistry Department, Faculty of Chemistry, Al.I Cuza University of Iasi, 700506 Iasi, Romania</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Laboratoire des Sciences du Climat et de l&apos;Environnement, CNRS/CEA, 91191 Gif-sur-Yvette Cedex, France</addr-line>
</aff>
<pub-date pub-type="epub">
<day>14</day>
<month>09</month>
<year>2007</year>
</pub-date>
<volume>7</volume>
<issue>17</issue>
<fpage>4661</fpage>
<lpage>4673</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/7/4661/2007/acp-7-4661-2007.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/7/4661/2007/acp-7-4661-2007.pdf</self-uri>
<abstract>
<p>In situ continuous hourly measurements of C&lt;sub&gt;2&lt;/sub&gt;&amp;ndash;C&lt;sub&gt;8&lt;/sub&gt; non-methane
hydrocarbons (NMHC&lt;sub&gt;&lt;I&gt;S&lt;/I&gt;&lt;/sub&gt;) have been performed from March to October 2006 at
two coastal locations (natural and rural) on the island of Crete, in the
Eastern Mediterranean. Well defined diel variations were observed for
several short lived NMHC&lt;sub&gt;&lt;I&gt;S&lt;/I&gt;&lt;/sub&gt; (including ethene, propene, n-butane,
n-pentane, n-hexane, 2-methyl-pentane). The daytime concentration of
hydroxyl (OH) radicals estimated from these experimental data varied from
1.3&amp;times;10&lt;sup&gt;6&lt;/sup&gt; to ~4.0&amp;times;10&lt;sup&gt;6&lt;/sup&gt; radical cm&lt;sup&gt;&amp;minus;3&lt;/sup&gt;, in
good agreement with box-model simulations. In addition the relative
variability of various hydrocarbon pairs (at least 7) was used to derive the
tropospheric levels of Cl atoms. The Cl atom concentration has been
estimated to range between 0.6&amp;times;10&lt;sup&gt;4&lt;/sup&gt; and 4.7&amp;times;10&lt;sup&gt;4&lt;/sup&gt; atom cm&lt;sup&gt;&amp;minus;3&lt;/sup&gt;,
in good agreement with gaseous hydrochloric acid (HCl)
observations in the area. Such levels of Cl atoms can be of considerable
importance for the oxidation capacity of the troposphere on a regional
scale.</p>
</abstract>
<counts><page-count count="13"/></counts>
</article-meta>
</front>
<body/>
<back>
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