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<article language="en">
	<journal>
		<journal_title>Atmospheric Chemistry and Physics Discussions</journal_title>
		<journal_url>www.atmos-chem-phys-discuss.net</journal_url>
		<issn>1680-7367</issn>
		<eissn>1680-7375</eissn>
		<volume_number>9</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/acpd-9-8159-2009</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/9/8159/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/9/8159/2009/acpd-9-8159-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/9/8159/2009/acpd-9-8159-2009.pdf</fulltext_pdf>
	<start_page>8159</start_page>
	<end_page>8185</end_page>
	<publication_date>2009-03-27</publication_date>
	<article_title content_type="html">Surface ozone trend details and interpretations in Beijing, 2001–2006</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>G. Tang</name>
		</author>
		<author numeration="2" affiliations="2">
			<name>X. Li</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>Y. Wang</name>
			<email>wys@dq.cern.ac.cn</email>
		</author>
		<author numeration="4" affiliations="1">
			<name>J. Xin</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>X. Ren</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, PR China</affiliation>
		<affiliation numeration="2" content_type="html">Beijing Municipal Environmental Protection Bureau, Beijing 100044, PR China</affiliation>
	</affiliations>
	<abstract content_type="html">Beijing is a megacity situated in the rapidly developing
Beijing-Tianjin-Hebei region of northern China. In this study, we analyze
data on ozone and nitrogen oxide levels obtained at six urban sites in
Beijing between the months of July and September. Our goal is to investigate
average trends and interpretations over the 2001–2006 period. Average
concentrations of NO&lt;sub&gt;x&lt;/sub&gt; (NO&lt;sub&gt;x&lt;/sub&gt;=NO+NO&lt;sub&gt;2&lt;/sub&gt;), O&lt;sub&gt;3&lt;/sub&gt;, and
O&lt;sub&gt;x&lt;/sub&gt; (O&lt;sub&gt;x&lt;/sub&gt;=O&lt;sub&gt;3&lt;/sub&gt;+NO&lt;sub&gt;2&lt;/sub&gt;) were 49.2&amp;plusmn;5.9 ppbv,
26.6&amp;plusmn;2.8 ppbv, and 60.3&amp;plusmn;1.9 ppbv, respectively. NO&lt;sub&gt;x&lt;/sub&gt;
concentrations decreased linearly at a rate of 3.9&amp;plusmn;0.5 ppbv/yr after
2002, while ozone concentrations increased at a rate of
1.1&amp;plusmn;0.5 ppbv/yr in a two-year cycle during 2001–2006, and O&lt;sub&gt;x&lt;/sub&gt;
concentrations remained nearly constant. The reduction of NO&lt;sub&gt;x&lt;/sub&gt;
emissions and elevated non-methane hydrocarbon (NMHCs) emissions may have
contributed to the increased O&lt;sub&gt;3&lt;/sub&gt; concentrations in Beijing. When the
contributions from Beijings urban and surrounding areas were disaggregated
via trajectory cluster analysis, daily maximum and average O&lt;sub&gt;x&lt;/sub&gt; concentrations
attributable to Beijing local emissions increased linearly at rates of
1.3&amp;plusmn;0.6 ppbv/yr and 0.8&amp;plusmn;0.6 ppbv/yr, while the O&lt;sub&gt;x&lt;/sub&gt; concentrations attributable
to regional areas decreased linearly at rates of 0.6&amp;plusmn;0.3 ppbv/yr and 0.5&amp;plusmn;0.3 ppbv/yr,
respectively. The decrease in O&lt;sub&gt;x&lt;/sub&gt; concentrations of surrounding areas
was found to counteract increasing Beijing urban O&lt;sub&gt;x&lt;/sub&gt; production, leading to
nearly constant O&lt;sub&gt;x&lt;/sub&gt; concentrations in the Beijing region over the study
period. Our results may be helpful for redefining government strategies to
control the photochemical formation of air pollutants in the Beijing region.
Our conclusions have relevance for developing megacities worldwide.</abstract>
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</article>

