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<article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" article-type="research-article" dtd-version="3.0" xml:lang="en">
<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-4-19-2004</article-id>
<title-group>
<article-title>Laboratory studies of the homogeneous nucleation of iodine oxides</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Burkholder</surname>
<given-names>J. 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>Curtius</surname>
<given-names>J.</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>Ravishankara</surname>
<given-names>A. R.</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>Lovejoy</surname>
<given-names>E. R.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Aeronomy Laboratory, National Oceanic and Atmospheric Administration, 325 Broadway, Boulder, CO 80305-3328, USA</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>now at: Institute for Atmospheric Physics, Mainz University, Mainz, Germany</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>also associated with the Dept. of Chemistry and Biochemistry, Uuniversity of Colorado, Boulder, CO 80309, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>20</day>
<month>01</month>
<year>2004</year>
</pub-date>
<volume>4</volume>
<issue>1</issue>
<fpage>19</fpage>
<lpage>34</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/4/19/2004/acp-4-19-2004.html">This article is available from http://www.atmos-chem-phys.net/4/19/2004/acp-4-19-2004.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/4/19/2004/acp-4-19-2004.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/4/19/2004/acp-4-19-2004.pdf</self-uri>
<abstract>
<p>Laboratory experimental results of iodine oxide nucleation are presented.
      Nucleation was induced following UV photolysis of CF&lt;sub&gt;3&lt;/sub&gt;I or CH&lt;sub&gt;2&lt;/sub&gt;I&lt;sub&gt;2&lt;/sub&gt; in
      the presence of excess ozone. Measurements were performed in a 70 L Teflon
      reactor with new particles detected using an Ultrafine Condensation Particle
      Counter, UCPC. The experimental results are interpreted using a coupled chemical
      - aerosol model to derive model parameters assuming single component homogeneous nucleation of OIO. The aerosol model results have been
      applied in an atmospheric box-model to interpret the possible implications of
      iodine oxide nucleation in the marine boundary layer. The model calculations
      demonstrate that IO and OIO concentrations reported in recent field measurements using long path absorption (Allan et al., 2000, 2001) are not
      sufficient to account for significant aerosol production either in the coastal or open ocean marine boundary layer using the mechanism presented. We
      demonstrate that inhomogeneous sources of iodine oxides, i.e.
      &amp;quot;hot&amp;quot; spots with elevated iodine species emissions, could account for the aerosol
      production bursts observed in the coastal region near Mace Head, Ireland.</p>
</abstract>
<counts><page-count count="16"/></counts>
</article-meta>
</front>
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