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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-10-10093-2010</article-id>
<title-group>
<article-title>Impact of transported background ozone inflow on summertime air quality in a California ozone exceedance area</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Parrish</surname>
<given-names>D. D.</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>Aikin</surname>
<given-names>K. 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>Oltmans</surname>
<given-names>S. J.</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>Johnson</surname>
<given-names>B. J.</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>Ives</surname>
<given-names>M.</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>Sweeny</surname>
<given-names>C.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>NOAA ESRL Chemical Sciences Division, 325 Broadway, Boulder, CO 80305, USA</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>CIRES, University of Colorado, Boulder, CO 80309, USA</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>NOAA ESRL Global Monitoring Division, 325 Broadway, Boulder, CO 80305, USA</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Humboldt State Marine Lab, 570 Ewing St., Trinidad Head, CA, 95570, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>27</day>
<month>10</month>
<year>2010</year>
</pub-date>
<volume>10</volume>
<issue>20</issue>
<fpage>10093</fpage>
<lpage>10109</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/10/10093/2010/acp-10-10093-2010.html">This article is available from http://www.atmos-chem-phys.net/10/10093/2010/acp-10-10093-2010.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/10/10093/2010/acp-10-10093-2010.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/10/10093/2010/acp-10-10093-2010.pdf</self-uri>
<abstract>
<p>Ozone sondes launched from Trinidad Head, California provide a measure of
background O&lt;sub&gt;3&lt;/sub&gt; transported ashore, and allow an evaluation of the impact
of this transport on air quality in California&apos;s Northern Sacramento Valley.
A strong summertime vertical O&lt;sub&gt;3&lt;/sub&gt; gradient and correlation analysis
indicate that O&lt;sub&gt;3&lt;/sub&gt;-rich air from above the marine boundary layer is
transported to the surface. Surface O&lt;sub&gt;3&lt;/sub&gt; is found to increase
proportionally to the transported background. At the surface site
experiencing the highest O&lt;sub&gt;3&lt;/sub&gt; concentrations, the mean maximum daily 8-h
average (MDA8) O&lt;sub&gt;3&lt;/sub&gt; on exceedance days (i.e. those days when MDA8 O&lt;sub&gt;3&lt;/sub&gt;
exceeds 75 ppbv) is 20 ppbv higher than on non-exceedance days. The
transported background O&lt;sub&gt;3&lt;/sub&gt;, as measured 22 h earlier by the Trinidad
Head sondes, accounts for more than half (11 ppbv) of this difference. This
finding contrasts with conclusions from model calculations that indicate the
US policy relevant O&lt;sub&gt;3&lt;/sub&gt; background is generally 15–35 ppbv, and that it
is lower, rather than higher, during pollution episodes. The present work
indicates that O&lt;sub&gt;3&lt;/sub&gt; transported on hemispheric scales substantially
impacts air quality in some areas of the US.</p>
</abstract>
<counts><page-count count="17"/></counts>
</article-meta>
</front>
<body/>
<back>
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