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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-11-9825-2011</article-id>
<title-group>
<article-title>Photochemical production of ozone in Beijing during the 2008 Olympic Games</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Chou</surname>
<given-names>C. C.-K.</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>Tsai</surname>
<given-names>C.-Y.</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>Chang</surname>
<given-names>C.-C.</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>Lin</surname>
<given-names>P.-H.</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>Liu</surname>
<given-names>S. C.</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>Zhu</surname>
<given-names>T.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Research Center for Environmental Changes, Academia Sinica, Taipei 11529, Taiwan</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Department of Atmospheric Sciences, National Taiwan University, Taipei 10617, Taiwan</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>College of Environmental Sciences and Engineering, Peking University, Beijing 100871, China</addr-line>
</aff>
<pub-date pub-type="epub">
<day>23</day>
<month>09</month>
<year>2011</year>
</pub-date>
<volume>11</volume>
<issue>18</issue>
<fpage>9825</fpage>
<lpage>9837</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/11/9825/2011/acp-11-9825-2011.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/11/9825/2011/acp-11-9825-2011.pdf</self-uri>
<abstract>
<p>As a part of the CAREBeijing-2008 campaign, observations of O&lt;sub&gt;3&lt;/sub&gt;, oxides
of nitrogen (NO&lt;sub&gt;x&lt;/sub&gt; and NO&lt;sub&gt;y&lt;/sub&gt;), CO, and hydrocarbons (NMHCs)
were carried out at the air quality observatory of the Peking University in
Beijing, China during August 2008, including the period of the 29th Summer
Olympic Games. The measurements were compared with those of the
CAREBeijing-2006 campaign to evaluate the effectiveness of the air pollution
control measures, which were conducted for improving the air quality in
Beijing during the Olympics. The results indicate that significant reduction
in the emissions of primary air pollutants had been achieved; the monthly
averaged mixing ratios of NO&lt;sub&gt;x&lt;/sub&gt;, NO&lt;sub&gt;y&lt;/sub&gt;, CO, and NMHCs decreased
by 42.2, 56.5, 27.8, and 49.7 %, respectively. In contrast to the primary
pollutants, the averaged mixing ratio of O&lt;sub&gt;3&lt;/sub&gt; increased by 42.2 %.
Nevertheless, it was revealed that the ambient levels of total oxidant
(O&lt;sub&gt;x&lt;/sub&gt; = O&lt;sub&gt;3&lt;/sub&gt;+NO&lt;sub&gt;2&lt;/sub&gt;+1.5 NO&lt;sub&gt;z&lt;/sub&gt;) and NO&lt;sub&gt;z&lt;/sub&gt; were
reduced by 21.3 and 77.4 %, respectively. The contradictions between
O&lt;sub&gt;3&lt;/sub&gt; and O&lt;sub&gt;x&lt;/sub&gt; were further examined in two case studies. Ozone
production rates of 30–70 ppbv h&lt;sup&gt;−1&lt;/sup&gt; and OPEx of ~8 
mole mole&lt;sup&gt;−1&lt;/sup&gt; were observed on a clear-sky day in spite of the reduced
levels of precursors. In that case, it was found that the mixing ratio of
O&lt;sub&gt;3&lt;/sub&gt; increased with the increasing NO&lt;sub&gt;2&lt;/sub&gt;/NO ratio, whereas the 
NO&lt;sub&gt;z&lt;/sub&gt; mixing ratio leveled off when NO&lt;sub&gt;2&lt;/sub&gt;/NO&gt;8. Consequently, the ratio of
O&lt;sub&gt;3&lt;/sub&gt; to NO&lt;sub&gt;z&lt;/sub&gt; increased to above 10, indicating the shift from
VOC-sensitive regime to NO&lt;sub&gt;x&lt;/sub&gt;-sensitive regime. However, in the other
case, it was found that the O&lt;sub&gt;3&lt;/sub&gt; production was inhibited significantly
due to substantial reduction in the NMHCs. According to the observations, it
was suggested that the O&lt;sub&gt;3&lt;/sub&gt; and/or O&lt;sub&gt;x&lt;/sub&gt; production rates in Beijing
should have been reduced as a result of the reduction in the emissions of
precursors during the Olympic period. However, the nighttime O&lt;sub&gt;3&lt;/sub&gt; levels
increased due to a decline in the NO-O&lt;sub&gt;3&lt;/sub&gt; titration, and the midday
O&lt;sub&gt;3&lt;/sub&gt; peak levels were elevated because of the shift in the photochemical
regime and the inhibition of NO&lt;sub&gt;z&lt;/sub&gt; formation.</p>
</abstract>
<counts><page-count count="13"/></counts>
</article-meta>
</front>
<body/>
<back>
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