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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>1</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/acpd-9-4805-2009</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/9/4805/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/9/4805/2009/acpd-9-4805-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/9/4805/2009/acpd-9-4805-2009.pdf</fulltext_pdf>
	<start_page>4805</start_page>
	<end_page>4871</end_page>
	<publication_date>2009-02-24</publication_date>
	<article_title content_type="html">Evaluating simulated primary anthropogenic and biomass burning organic aerosols during MILAGRO: implications for assessing treatments of secondary organic aerosols</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>J. D. Fast</name>
		</author>
		<author numeration="2" affiliations="2">
			<name>A. C. Aiken</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>J. Allan</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>L. Alexander</name>
		</author>
		<author numeration="5" affiliations="4">
			<name>T. Campos</name>
		</author>
		<author numeration="6" affiliations="5">
			<name>M. R. Canagaratna</name>
		</author>
		<author numeration="7" affiliations="1">
			<name>E. Chapman</name>
		</author>
		<author numeration="8" affiliations="6">
			<name>P. F. DeCarlo</name>
		</author>
		<author numeration="9" affiliations="7">
			<name>B. de Foy</name>
		</author>
		<author numeration="10" affiliations="8">
			<name>J. Gaffney</name>
		</author>
		<author numeration="11" affiliations="9">
			<name>J. de Gouw</name>
		</author>
		<author numeration="12" affiliations="1">
			<name>J. C. Doran</name>
		</author>
		<author numeration="13" affiliations="4">
			<name>L. Emmons</name>
		</author>
		<author numeration="14" affiliations="4">
			<name>A. Hodzic</name>
		</author>
		<author numeration="15" affiliations="5">
			<name>S. C. Herndon</name>
		</author>
		<author numeration="16" affiliations="10">
			<name>G. Huey</name>
		</author>
		<author numeration="17" affiliations="5">
			<name>J. T. Jayne</name>
		</author>
		<author numeration="18" affiliations="2">
			<name>J. L. Jimenez</name>
		</author>
		<author numeration="19" affiliations="11">
			<name>L. Kleinman</name>
		</author>
		<author numeration="20" affiliations="9">
			<name>W. Kuster</name>
		</author>
		<author numeration="21" affiliations="8">
			<name>N. Marley</name>
		</author>
		<author numeration="22" affiliations="12">
			<name>L. Russell</name>
		</author>
		<author numeration="23" affiliations="13">
			<name>C. Ochoa</name>
		</author>
		<author numeration="24" affiliations="5">
			<name>T. B. Onasch</name>
		</author>
		<author numeration="25" affiliations="1">
			<name>M. Pekour</name>
		</author>
		<author numeration="26" affiliations="1">
			<name>C. Song</name>
		</author>
		<author numeration="27" affiliations="2">
			<name>I. M. Ulbrich</name>
		</author>
		<author numeration="28" affiliations="9">
			<name>C. Warneke</name>
		</author>
		<author numeration="29" affiliations="9">
			<name>D. Welsh-Bon</name>
		</author>
		<author numeration="30" affiliations="4">
			<name>C. Wiedinmyer</name>
		</author>
		<author numeration="31" affiliations="5">
			<name>D. R. Worsnop</name>
		</author>
		<author numeration="32" affiliations="1">
			<name>X.-Y. Yu</name>
		</author>
		<author numeration="33" affiliations="1">
			<name>R. Zaveri</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Pacific Northwest National Laboratory, Richland, Washington, USA</affiliation>
		<affiliation numeration="2" content_type="html">University of Colorado, Boulder Colorado, USA</affiliation>
		<affiliation numeration="3" content_type="html">University of Manchester, Manchester, UK</affiliation>
		<affiliation numeration="4" content_type="html">National Center for Atmospheric Research, Boulder, Colorado, USA</affiliation>
		<affiliation numeration="5" content_type="html">Aerodyne Research Inc., Billerica, Massachusetts, USA</affiliation>
		<affiliation numeration="6" content_type="html">Paul Scherrer Institut, Switzerland</affiliation>
		<affiliation numeration="7" content_type="html">Saint Louis University, Saint Louis, Missouri, USA</affiliation>
		<affiliation numeration="8" content_type="html">University of Arkansas â€“ Little Rock, Little Rock, Arkansas, USA</affiliation>
		<affiliation numeration="9" content_type="html">NOAA Earth System Research Laboratory &amp; Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, Colorado, USA</affiliation>
		<affiliation numeration="10" content_type="html">Georgia Institute of Technology, Atlanta, Georgia, USA</affiliation>
		<affiliation numeration="11" content_type="html">Brookhaven National Laboratory, Upton, New York, USA</affiliation>
		<affiliation numeration="12" content_type="html">University of California â€“ San Diego, San Diego, California, USA</affiliation>
		<affiliation numeration="13" content_type="html">Universidad Nacional Aut Â´onoma de MÂ´exico, Mexico City, Mexico</affiliation>
	</affiliations>
	<abstract content_type="html">Simulated primary organic aerosols (POA), as well as other particulates and
trace gases, in the vicinity of Mexico City are evaluated using measurements
collected during the 2006 Megacity Initiative: Local and Global Research
Observations (MILAGRO) field campaigns. Since the emission inventories and
dilution will directly affect predictions of total organic matter and
consequently total particulate matter, our objective is to assess the
uncertainties in predicted POA before testing and evaluating the performance
of secondary organic aerosol (SOA) treatments. Carbon monoxide (CO) is well
simulated on most days both over the city and downwind, indicating that
transport and mixing processes were usually consistent with the
meteorological conditions observed during MILAGRO. Predicted and observed
elemental carbon (EC) in the city was similar, but larger errors occurred at
remote locations since the overall CO/EC emission ratios in the national
emission inventory were lower than in the metropolitan emission inventory.
Components of organic aerosols derived from Positive Matrix Factorization of
data from several Aerodyne Aerosol Mass Spectrometer instruments deployed
both at ground sites and on research aircraft are used to evaluate the
model. Modeled POA was consistently lower than the measured organic matter
at the ground sites, which is consistent with the expectation that SOA
should be a large fraction of the total organic matter mass. A much better
agreement was found when modeled POA was compared with the sum of measured
&quot;primary anthropogenic&quot; and &quot;biomass burning&quot; components on most days,
suggesting that the overall magnitude of primary organic particulates
released was reasonable. The modeled POA was greater than the total observed
organic matter when the aircraft flew directly downwind of large fires,
suggesting that biomass burning emission estimates from some large fires may
be too high. Predicted total observed organic carbon (TOOC) was also
analyzed to assess how emission inventory estimates of volatile organic
compounds may impact predictions of SOA.</abstract>
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</article>

