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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>8</volume_number>
		<issue_number>4</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/acpd-8-15739-2008</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/8/15739/2008/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/8/15739/2008/acpd-8-15739-2008.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/8/15739/2008/acpd-8-15739-2008.pdf</fulltext_pdf>
	<start_page>15739</start_page>
	<end_page>15789</end_page>
	<publication_date>2008-08-19</publication_date>
	<article_title content_type="html">Ozone production, nitrogen oxides, and radical budgets in Mexico City: observations from Pico de Tres Padres</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>E. C. Wood</name>
			<email>ezrawood@aerodyne.com</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>S. C. Herndon</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>T. B. Onasch</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>J. H. Kroll</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>M. R. Canagaratna</name>
		</author>
		<author numeration="6" affiliations="1">
			<name>C. E. Kolb</name>
		</author>
		<author numeration="7" affiliations="1">
			<name>D. R. Worsnop</name>
		</author>
		<author numeration="8" affiliations="2">
			<name>J. A. Neuman</name>
		</author>
		<author numeration="9" affiliations="3">
			<name>R. Seila</name>
		</author>
		<author numeration="10" affiliations="4">
			<name>M. Zavala</name>
		</author>
		<author numeration="11" affiliations="5">
			<name>W. B. Knighton</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Aerodyne Research, Inc., Billerica, Massachusetts, USA</affiliation>
		<affiliation numeration="2" content_type="html">Earth System Research Laboratory, NOAA, Boulder, Colorado, USA</affiliation>
		<affiliation numeration="3" content_type="html">National Exposure Research Laboratory, Environmental Protection Agency, Research Triangle Park, North Carolina, USA</affiliation>
		<affiliation numeration="4" content_type="html">Molina Center for Energy and the Environment, La Jolla, California, USA</affiliation>
		<affiliation numeration="5" content_type="html">Dept. of Chemistry and Biochemistry, Montana State University, Bozeman, Montana, USA</affiliation>
	</affiliations>
	<abstract content_type="html">Observations at a mountain-top site within the Mexico City basin are used to
characterize ozone production and destruction, the nitrogen oxide budget,
and the radical budget during the MILAGRO campaign. An ozone production rate
of ~50 ppbv/h was observed in a stagnant air mass during the
afternoon of 12 March 2006, which is among the highest observed anywhere in
the world. Approximately half of the ozone destruction was due to the
oxidation of NO&lt;sub&gt;2&lt;/sub&gt;. During this time period ozone production was
VOC-limited, deduced by a comparison of the radical production rates and the
formation rate of NO&lt;sub&gt;x&lt;/sub&gt; oxidation products (NO&lt;sub&gt;z&lt;/sub&gt;) For
[NO&lt;sub&gt;x&lt;/sub&gt;]/[NO&lt;sub&gt;y&lt;/sub&gt;] values between 0.2 and 0.8, gas-phase HNO&lt;sub&gt;3&lt;/sub&gt;
typically accounted for less than 10% of NO&lt;sub&gt;z&lt;/sub&gt; and accumulation-mode
particulate nitrate (NO&lt;sub&gt;3&lt;/sub&gt;&lt;sup&gt;&amp;minus;&lt;/sup&gt;&lt;sub&gt;(PM)&lt;/sub&gt;) accounted for 20%–70%
of NO&lt;sub&gt;z&lt;/sub&gt;, consistent with high ambient NH&lt;sub&gt;3&lt;/sub&gt; concentrations. The
fraction of NO&lt;sub&gt;z&lt;/sub&gt; accounted for by the sum of HNO&lt;sub&gt;3(g)&lt;/sub&gt; and
NO&lt;sub&gt;3&lt;/sub&gt;&lt;sup&gt;&amp;minus;&lt;/sup&gt;&lt;sub&gt;(PM)&lt;/sub&gt; decreased with photochemical processing. This
decrease is apparent even when dry deposition of HNO&lt;sub&gt;3&lt;/sub&gt; is accounted for,
and indicates that HNO&lt;sub&gt;3&lt;/sub&gt; formation decreased relative to other NO&lt;sub&gt;x&lt;/sub&gt;
&quot;sink&quot; processes during the first 12 h of photochemistry and/or a
significant fraction of the nitrate was associated with the coarse aerosol
size mode. The ozone production efficiency of NO&lt;sub&gt;x&lt;/sub&gt; on 11 and 12 March
2006 was approximately 7 on a time scale of one day. A new metric for ozone
production efficiency that relates the dilution-adjusted ozone mixing ratio
to cumulative OH exposure is proposed.</abstract>
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</article>

