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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>10</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/acpd-10-3457-2010</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/10/3457/2010/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/10/3457/2010/acpd-10-3457-2010.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/10/3457/2010/acpd-10-3457-2010.pdf</fulltext_pdf>
	<start_page>3457</start_page>
	<end_page>3498</end_page>
	<publication_date>2010-02-09</publication_date>
	<article_title content_type="html">Impact of Mexico City emissions on regional air quality from MOZART-4 simulations</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>L. K. Emmons</name>
			<email>emmons@ucar.edu</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>E. C. Apel</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>J.-F. Lamarque</name>
		</author>
		<author numeration="4" affiliations="1,11">
			<name>P. G. Hess</name>
		</author>
		<author numeration="5" affiliations="2">
			<name>M. Avery</name>
		</author>
		<author numeration="6" affiliations="3">
			<name>D. Blake</name>
		</author>
		<author numeration="7" affiliations="4">
			<name>W. Brune</name>
		</author>
		<author numeration="8" affiliations="1">
			<name>T. Campos</name>
		</author>
		<author numeration="9" affiliations="2">
			<name>J. Crawford</name>
		</author>
		<author numeration="10" affiliations="5,12">
			<name>P. F. DeCarlo</name>
		</author>
		<author numeration="11" affiliations="1">
			<name>S. Hall</name>
		</author>
		<author numeration="12" affiliations="6">
			<name>B. Heikes</name>
		</author>
		<author numeration="13" affiliations="7">
			<name>J. Holloway</name>
		</author>
		<author numeration="14" affiliations="5">
			<name>J. L. Jimenez</name>
		</author>
		<author numeration="15" affiliations="1">
			<name>D. J. Knapp</name>
		</author>
		<author numeration="16" affiliations="8">
			<name>G. Kok</name>
		</author>
		<author numeration="17" affiliations="9,13,14">
			<name>M. Mena-Carrasco</name>
		</author>
		<author numeration="18" affiliations="2">
			<name>J. Olson</name>
		</author>
		<author numeration="19" affiliations="10">
			<name>D. O&apos;Sullivan</name>
		</author>
		<author numeration="20" affiliations="2">
			<name>G. Sachse</name>
		</author>
		<author numeration="21" affiliations="1">
			<name>J. Walega</name>
		</author>
		<author numeration="22" affiliations="1">
			<name>P. Weibring</name>
		</author>
		<author numeration="23" affiliations="1">
			<name>A. Weinheimer</name>
		</author>
		<author numeration="24" affiliations="1">
			<name>C. Wiedinmyer</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">National Center for Atmospheric Research, Boulder, CO, USA</affiliation>
		<affiliation numeration="2" content_type="html">NASA Langley Research Center, Hampton, VA, USA</affiliation>
		<affiliation numeration="3" content_type="html">Department of Chemistry, University of California, Irvine, CA, USA</affiliation>
		<affiliation numeration="4" content_type="html">Department of Meteorology, Pennsylvania State University, University Park, PA, USA</affiliation>
		<affiliation numeration="5" content_type="html">Department of Chemistry and Biochemistry, University of Colorado, Boulder, CO, USA</affiliation>
		<affiliation numeration="6" content_type="html">Graduate School of Oceanography, University of Rhode Island, Narragansett, RI, USA</affiliation>
		<affiliation numeration="7" content_type="html">NOAA, Earth System Research Laboratory, Boulder, CO, USA and Cooperative Institute for Research in Environmental Science, University of Colorado, Boulder, CO, USA</affiliation>
		<affiliation numeration="8" content_type="html">Droplet Measurement Technologies, Boulder, CO, USA</affiliation>
		<affiliation numeration="9" content_type="html">University of Iowa, IA, USA</affiliation>
		<affiliation numeration="10" content_type="html">Chemistry Department, US Naval Academy, Annapolis, MD, USA</affiliation>
		<affiliation numeration="11" content_type="html">now at: Department of Biological and Environmental Engineering, Cornell University, Ithaca, NY, USA</affiliation>
		<affiliation numeration="12" content_type="html">now at: Laboratory of Atmospheric Chemistry, Paul Scherrer Institut, Villigen, Switzerland</affiliation>
		<affiliation numeration="13" content_type="html">now at: Universidad Andrés Bello, Santiago, Chile</affiliation>
		<affiliation numeration="14" content_type="html">now at: Massachusetts Institute of Technology, Cambridge, MA, USA</affiliation>
	</affiliations>
	<abstract content_type="html">An extensive set of measurements was made in and around Mexico City as
      part of the MILAGRO (Megacity Initiative: Local and Global Research
      Observations) experiments in March 2006.  Simulations with the Model
      for Ozone and Related Chemical Tracers, version 4 (MOZART-4), a global
      chemical transport model, have been used to provide a regional context
      for these observations and assist in their interpretation.  These
      MOZART-4 simulations reproduce the aircraft observations generally
      well, but some differences in the modeled volatile organic compounds
      (VOCs) from the observations result from incorrect VOC speciation
      assumed for the emission inventories.  The different types of
CO sources represented in the model have been &amp;quot;tagged&amp;quot; to
      quantify the contributions of regions outside Mexico, as well as the
      various emissions sectors within Mexico, to the regional air quality
      of Mexico.  This analysis indicates open fires have some, but not
      a dominant, impact on the atmospheric composition in the region around
      Mexico City, when averaged over the month.  However, considerable
      variation in the fire contribution (2–15% of total CO) is seen
      during the month.  The transport and photochemical aging of Mexico
      City emissions were studied using tags of CO emissions for each
      day, showing that typically the air near Mexico City was a combination
      of many ages.  Ozone production in MOZART-4 is shown to agree well
      with the net production rates from box model calculations constrained
      by the MILAGRO aircraft measurements.  Ozone production efficiency
      derived from the ratio of O&lt;sub&gt;x&lt;/sub&gt; to NO&lt;sub&gt;z&lt;/sub&gt; is higher in
      MOZART-4 than in the observations for moderately polluted air.  OH
      reactivity determined from the MOZART-4 results shows the same
      increase in relative importance of oxygenated VOCs downwind of Mexico
      City as the reactivity inferred from the observations.  The amount of
      ozone produced by emissions from Mexico City and surrounding areas has
      been quantified in the model by tracking NO emissions, showing
      little influence beyond Mexico&apos;s borders, and also relatively minor
      influence from fire emissions on the monthly average tropospheric
      ozone column.</abstract>
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</article>

