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<article language="en">
	<journal>
		<journal_title>Atmospheric Chemistry and Physics</journal_title>
		<journal_url>www.atmos-chem-phys.net</journal_url>
		<issn>1680-7316</issn>
		<eissn>1680-7324</eissn>
		<volume_number>9</volume_number>
		<issue_number>18</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/acp-9-6655-2009</doi>
	<article_url>http://www.atmos-chem-phys.net/9/6655/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys.net/9/6655/2009/acp-9-6655-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys.net/9/6655/2009/acp-9-6655-2009.pdf</fulltext_pdf>
	<start_page>6655</start_page>
	<end_page>6675</end_page>
	<publication_date>2009-09-15</publication_date>
	<article_title content_type="html">Measurements of OH and HO&lt;sub&gt;2&lt;/sub&gt; concentrations during the MCMA-2006 field campaign â€“ Part 2: Model comparison and radical budget</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>S. Dusanter</name>
			<email>sdusante@indiana.edu</email>
		</author>
		<author numeration="2" affiliations="1,14">
			<name>D. Vimal</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>P. S. Stevens</name>
		</author>
		<author numeration="4" affiliations="2">
			<name>R. Volkamer</name>
		</author>
		<author numeration="5" affiliations="3,4">
			<name>L. T. Molina</name>
		</author>
		<author numeration="6" affiliations="5">
			<name>A. Baker</name>
		</author>
		<author numeration="7" affiliations="5">
			<name>S. Meinardi</name>
		</author>
		<author numeration="8" affiliations="5">
			<name>D. Blake</name>
		</author>
		<author numeration="9" affiliations="3,4">
			<name>P. Sheehy</name>
		</author>
		<author numeration="10" affiliations="6,15">
			<name>A. Merten</name>
		</author>
		<author numeration="11" affiliations="7">
			<name>R. Zhang</name>
		</author>
		<author numeration="12" affiliations="7">
			<name>J. Zheng</name>
		</author>
		<author numeration="13" affiliations="8,16">
			<name>E. C. Fortner</name>
		</author>
		<author numeration="14" affiliations="9">
			<name>W. Junkermann</name>
		</author>
		<author numeration="15" affiliations="10">
			<name>M. Dubey</name>
		</author>
		<author numeration="16" affiliations="10">
			<name>T. Rahn</name>
		</author>
		<author numeration="17" affiliations="11">
			<name>B. Eichinger</name>
		</author>
		<author numeration="18" affiliations="11">
			<name>P. Lewandowski</name>
		</author>
		<author numeration="19" affiliations="12">
			<name>J. Prueger</name>
		</author>
		<author numeration="20" affiliations="13">
			<name>H. Holder</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Center for Research in Environmental Science, School of Public and Environmental Affairs, and Department of Chemistry, Indiana University, Bloomington, IN 47405, USA</affiliation>
		<affiliation numeration="2" content_type="html">Department of Chemistry and Biochemistry, University of Colorado, USA</affiliation>
		<affiliation numeration="3" content_type="html">Molina Center for Energy and the Environment USA</affiliation>
		<affiliation numeration="4" content_type="html">Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, USA</affiliation>
		<affiliation numeration="5" content_type="html">University of California, Irvine, 92697 CA, USA</affiliation>
		<affiliation numeration="6" content_type="html">Institute of Environmental Physics, University of Heidelberg, Germany</affiliation>
		<affiliation numeration="7" content_type="html">Department of Atmospheric Sciences, Texas A&amp;M University, USA</affiliation>
		<affiliation numeration="8" content_type="html">Department of Chemistry, Montana State University, USA</affiliation>
		<affiliation numeration="9" content_type="html">Forschungszentrum Karlsruhe, Institute of Meteorology and Climate Research, IMK-IFU, Garmisch-Partenkirchen, Germany</affiliation>
		<affiliation numeration="10" content_type="html">Earth and Environmental Sciences Division, Los Alamos National Laboratory, USA</affiliation>
		<affiliation numeration="11" content_type="html">IIHR-Hydroscience &amp; Engineering, University of Iowa, Iowa City, IA, USA</affiliation>
		<affiliation numeration="12" content_type="html">USDA National Soil Tilth Lab, Ames, IA, USA</affiliation>
		<affiliation numeration="13" content_type="html">Duke University, Durham, NC, USA</affiliation>
		<affiliation numeration="14" content_type="html">now at: SRI International, Menlo Park, CA, USA</affiliation>
		<affiliation numeration="15" content_type="html">now at: Institute of Applied Photophysics, Dresden University of Technology, Germany</affiliation>
		<affiliation numeration="16" content_type="html">now at: Aerodyne Research Incorporated, 45 Manning Road, Billerica, MA, USA</affiliation>
	</affiliations>
	<abstract content_type="html">Measurements of hydroxyl (OH) and hydroperoxy (HO&lt;sub&gt;2&lt;/sub&gt;) radicals were made
during the Mexico City Metropolitan Area (MCMA) field campaign as part of
the MILAGRO (Megacity Initiative: Local and Global Research Observations)
project during March 2006. These measurements provide a unique opportunity
to test current models of atmospheric RO&lt;sub&gt;x&lt;/sub&gt; (OH + HO&lt;sub&gt;2&lt;/sub&gt; + RO&lt;sub&gt;2&lt;/sub&gt;)
photochemistry under polluted conditions. A zero-dimensional box model based
on the Regional Atmospheric Chemical Mechanism (RACM) was constrained by
10-min averages of 24 &lt;i&gt;J&lt;/i&gt;-values and the concentrations of 97 chemical
species. Several issues related to the RO&lt;sub&gt;x&lt;/sub&gt; chemistry under polluted
conditions are highlighted in this study: (i) Measured concentrations of
both OH and HO&lt;sub&gt;2&lt;/sub&gt; were underpredicted during morning hours on a median
campaign basis, suggesting a significant source of radicals is missing from
current atmospheric models under polluted conditions, consistent with
previous urban field campaigns. (ii) The model-predicted HO&lt;sub&gt;2&lt;/sub&gt;/OH ratios
underestimate the measurements for NO mixing ratios higher than 5 ppb, also
consistent with previous urban field campaigns. This suggests that under
high NO&lt;sub&gt;x&lt;/sub&gt; conditions, the HO&lt;sub&gt;2&lt;/sub&gt; to OH propagation rate may be
overestimated by the model or a process converting OH into HO&lt;sub&gt;2&lt;/sub&gt; may be
missing from the chemical mechanism. On a daily basis (08:40 a.m.â€“06:40 p.m.),
an analysis of the radical budget indicates that HONO photolysis, HCHO
photolysis, O&lt;sub&gt;3&lt;/sub&gt;-alkene reactions and dicarbonyls photolysis are the main
radical sources. O&lt;sub&gt;3&lt;/sub&gt; photolysis contributes to less than 6% of the
total radical production.</abstract>
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</article>

