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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>6</volume_number>
		<issue_number>5</issue_number>
		<publication_year>2006</publication_year>
	</journal>
	<doi>10.5194/acpd-6-8961-2006</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/6/8961/2006/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/6/8961/2006/acpd-6-8961-2006.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/6/8961/2006/acpd-6-8961-2006.pdf</fulltext_pdf>
	<start_page>8961</start_page>
	<end_page>9002</end_page>
	<publication_date>2006-09-25</publication_date>
	<article_title content_type="html">Ozone production and hydrocarbon reactivity in Hong Kong, Southern China</article_title>
	<authors>
		<author numeration="1" affiliations="1,2">
			<name>J. Zhang</name>
		</author>
		<author numeration="2" affiliations="3">
			<name>T. Wang</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>W. L. Chameides</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>C. Cardelino</name>
		</author>
		<author numeration="5" affiliations="3">
			<name>J. Kwok</name>
		</author>
		<author numeration="6" affiliations="4">
			<name>D. R. Blake</name>
		</author>
		<author numeration="7" affiliations="3">
			<name>A. Ding</name>
		</author>
		<author numeration="8" affiliations="3">
			<name>K. L. So</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, GA 30332, USA</affiliation>
		<affiliation numeration="2" content_type="html">School of Geography, Beijing Normal University, Beijing 100875, China</affiliation>
		<affiliation numeration="3" content_type="html">Department of Civil and Structural Engineering, Hong Kong Polytechnic University, HongKong, China</affiliation>
		<affiliation numeration="4" content_type="html">Department of Chemistry, University of California, Irvine, CA 92697, USA</affiliation>
	</affiliations>
	<abstract content_type="html">Data obtained in Hong Kong during the Hong Kong and the Pearl River Delta
(PRD) Pilot Air Monitoring Study in autumn 2002 are analyzed to unravel the
relationship between ground-level ozone (O&lt;sub&gt;3&lt;/sub&gt;), pollution precursors, and
cross-border transport. Ten ozone episodes, during which the hourly O&lt;sub&gt;3&lt;/sub&gt; concentration exceeded 100 ppbv in 9 cases and 90 ppbv in one case, are
subject to detailed analysis, including one case with hourly O&lt;sub&gt;3&lt;/sub&gt; of 203
ppbv, which is the highest concentration on record to date in Hong Kong.
Combined with high-resolution back trajectories, dCO/dNO&lt;sub&gt;&lt;i&gt;y&lt;/i&gt;&lt;/sub&gt; is used to
define whether O&lt;sub&gt;3&lt;/sub&gt; is locally or regionally produced. Five out of the
ten Hong Kong O&lt;sub&gt;3&lt;/sub&gt;-episodes studied show a &apos;&apos;pollution signature&apos;&apos; that
is indicative of impact from Guangdong Province. Examination of speciated
volatile organic compounds (VOCs) shows that the reactivity of VOCs is
dominated by anthropogenic VOCs, of which the reactive aromatics dominate,
in particular xylenes and toluene. Calculations using a photochemical box
model indicate that between 50&amp;ndash;100% of the O&lt;sub&gt;3&lt;/sub&gt; increase observed in
Hong Kong during the O&lt;sub&gt;3&lt;/sub&gt; episodes can be explained by photochemical
generation within the Hong Kong area, provided that nitrous acid (HONO) is
present at the concentrations derived from this study. An Observation-Based
Model (OBM) is used to calculate the sensitivity of the O&lt;sub&gt;3&lt;/sub&gt; production
to changes in the concentrations of the precursor compounds. Generally the
production of O&lt;sub&gt;3&lt;/sub&gt; throughout much of the Hong Kong area is limited by
VOCs, while high nitric oxide (NO) concentrations suppress O&lt;sub&gt;3&lt;/sub&gt;
concentration.</abstract>
	<references>
	</references>
</article>

