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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>GÃ¶ttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acp-8-6355-2008</article-id>
<title-group>
<article-title>Variations of O&lt;sub&gt;3&lt;/sub&gt; and CO in summertime at a rural site near Beijing</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Wang</surname>
<given-names>Y.</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>McElroy</surname>
<given-names>M. 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>Munger</surname>
<given-names>J. W.</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>Hao</surname>
<given-names>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>Ma</surname>
<given-names>H.</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>Nielsen</surname>
<given-names>C. P.</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>Chen</surname>
<given-names>Y.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Department of Environmental Science and Engineering, Tsinghua University, Beijing, China</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Department of Earth and Planetary Sciences and School of Engineering and Applied Sciences, Harvard Univ., Cambridge, Massachusetts, USA</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Harvard China Project and School of Engineering and Applied Sciences, Harvard Univ., Cambridge, Massachusetts, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>05</day>
<month>11</month>
<year>2008</year>
</pub-date>
<volume>8</volume>
<issue>21</issue>
<fpage>6355</fpage>
<lpage>6363</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/8/6355/2008/acp-8-6355-2008.html">This article is available from http://www.atmos-chem-phys.net/8/6355/2008/acp-8-6355-2008.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/8/6355/2008/acp-8-6355-2008.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/8/6355/2008/acp-8-6355-2008.pdf</self-uri>
<abstract>
<p>Large intra-season differences in mixing ratios of CO and O&lt;sub&gt;3&lt;/sub&gt; were
detected at Miyun, a rural site north of Beijing, in summer 2006. Despite an
increase in mean daytime mixing ratio of CO from 500 ppbv in June to 700
ppbv in July, mean daytime O&lt;sub&gt;3&lt;/sub&gt; dropped from 67 ppbv in June to 50 ppbv
in July and August. The observed changes in CO and O&lt;sub&gt;3&lt;/sub&gt; are attributed to
the influence of the summer monsoonal circulation that develops over the
North China Plain in July. Photochemical production of O&lt;sub&gt;3&lt;/sub&gt; is reduced as
a consequence of increased cloudiness during July and August, as indicated
by the strong negative correlation observed between O&lt;sub&gt;3&lt;/sub&gt; and satellite
observations of cloud optical depth, with cloudiness having little effect on
CO. The analysis suggests a strategy for emission controls that could be
implemented in an economically efficient manner to minimize the frequency of
high levels of O&lt;sub&gt;3&lt;/sub&gt; during summer in Beijing.</p>
</abstract>
<counts><page-count count="9"/></counts>
</article-meta>
</front>
<body/>
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