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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ACPD</journal-id>
<journal-title-group>
<journal-title>Atmospheric Chemistry and Physics Discussions</journal-title>
<abbrev-journal-title abbrev-type="publisher">ACPD</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Atmos. Chem. Phys. Discuss.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7375</issn>
<publisher><publisher-name></publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acp-2016-508</article-id>
<title-group>
<article-title>Characteristics of Ground Ozone Concentration over Beijing from 2004 to
2015: Trends, Transport, and Effects of Reductions</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Cheng</surname>
<given-names>Nianliang</given-names>
<ext-link>https://orcid.org/0000-0002-7981-9128</ext-link>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</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>Li</surname>
<given-names>Yunting</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>Zhang</surname>
<given-names>Dawei</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Chen</surname>
<given-names>Tian</given-names>
</name>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Sun</surname>
<given-names>Feng</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff6">
<sup>6</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Chen</surname>
<given-names>Chen</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff6">
<sup>6</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Meng</surname>
<given-names>Fan</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Beijing Key Laboratory of Airborne Particulate Matter Monitoring Technology, Beijing Municipal Environmental Monitoring Center, Beijing 100048, China</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>College of Water Sciences, Beijing Normal University, Beijing 100875, China</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>State Key Laboratory of Environmental Criteria and Risk Assessment, Chinese Research Academy of Environmental Sciences, Beijing 100012, China</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Department of Environmental Science and Engineering,Tsinghua University, Beijing 100084, China</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>Beijing Municipal Environmental Protection Bureau, Beijing 100044, China</addr-line>
</aff>
<aff id="aff6">
<label>6</label>
<addr-line>Department of Environmental Science, Peking University, Beijing 100871, China</addr-line>
</aff>
<pub-date pub-type="epub">
<day>10</day>
<month>08</month>
<year>2016</year>
</pub-date>
<volume>2016</volume>
<fpage>1</fpage>
<lpage>21</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2016 Nianliang Cheng et al.</copyright-statement>
<copyright-year>2016</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 3.0 Unported License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by/3.0/">https://creativecommons.org/licenses/by/3.0/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://acp.copernicus.org/preprints/acp-2016-508/">This article is available from https://acp.copernicus.org/preprints/acp-2016-508/</self-uri>
<self-uri xlink:href="https://acp.copernicus.org/preprints/acp-2016-508/acp-2016-508.pdf">The full text article is available as a PDF file from https://acp.copernicus.org/preprints/acp-2016-508/acp-2016-508.pdf</self-uri>
<abstract>
<p>Based on the  hourly ozone monitoring data during 2004&amp;ndash;2015 in urban area and at DL background station in Beijing, a comprehensive discussion of the characteristics of ozone concentration was conducted. Annual concentration of daily maximum 1&amp;thinsp;h ozone (O&lt;sub&gt;3&lt;/sub&gt; 1&amp;thinsp;h) was all increasing at urban sites (1.79&amp;thinsp;ppbv&amp;thinsp;yr&lt;sup&gt;&amp;minus;1&lt;/sup&gt;) and DL background station (2.05&amp;thinsp;ppbv&amp;thinsp;yr&lt;sup&gt;&amp;minus;1&lt;/sup&gt;) while daily maximum 8&amp;thinsp;h average ozone concentration (O&lt;sub&gt;3&lt;/sub&gt; 8&amp;thinsp;h) was increasing in urban area (1.14&amp;thinsp;ppbv&amp;thinsp;yr&lt;sup&gt;&amp;minus;1&lt;/sup&gt;) and slightly decreasing at DL background station (&amp;minus;0.47&amp;thinsp;ppbv&amp;thinsp;yr&lt;sup&gt;&amp;minus;1&lt;/sup&gt;) from 2004 to 2015 due to different ozone sensitivity regimes and ratios of NO&lt;sub&gt;2&lt;/sub&gt;/NO. Diurnal variation of ozone peaks obtained at downwind DL station were about 1&amp;thinsp;h later than that in urban area from May to October in different years and concentration of ozone at a DL background station was much higher than that of urban sites. Moreover, the difference of ozone peaks between urban sites and DL background station was significantly becoming smaller in recent years, which may be related to the regional ozone transport and the expansion urbanization of Beijing. Based on the joint efforts of regional air pollution prevention and control,Beijing achieved Sep 3 military blue. Calculated average concentrations of CO, NO&lt;sub&gt;2&lt;/sub&gt;, and O&lt;sub&gt;3&lt;/sub&gt; in S2 (Aug 20~31, 2015) and S3 (Sep 01~03, 2015) decreased by 31.48&amp;thinsp;%, 43.97&amp;thinsp;%, and 13.21&amp;thinsp;% at urban sites, and by 20.93&amp;thinsp;%, 57.10&amp;thinsp;%, and 23.62&amp;thinsp;% at DL station, respectively compared with those in S1 (Aug 01~19,2015) and S4 Sep 04~30, 2015). A reduction of local anthropogenic emissions such as VOCs  and NOx could reduce ozone efficiently especially in downwind areas of Beijing and made the ozone peaks decrease significantly and appear 2~3&amp;thinsp;h earlier compared to the scenarios of no emission reductions. Compared to the increasing ozone during Asia-Pacific Economic Cooperation (APEC)meeting period,to decrease the ozone concentration in Beijing, VOCs emissions should be reduced larger and be controlled stricter than that of NO&lt;sub&gt;&lt;i&gt;x&lt;/i&gt;&lt;/sub&gt; in Beijing and the policy of regional air pollution joint prevention and control should still be promoted unswervingly and jointly in the further.</p>
</abstract>
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<award-group id="gs1">
<funding-source></funding-source>
<award-id>201409005</award-id>
</award-group>
</funding-group>
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