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<!DOCTYPE article SYSTEM "http://www.atmos-chem-phys-discuss.net/inc/acpd/copernicus.dtd">
<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>5</volume_number>
		<issue_number>3</issue_number>
		<publication_year>2005</publication_year>
	</journal>
	<doi>10.5194/acpd-5-4183-2005</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/5/4183/2005/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/5/4183/2005/acpd-5-4183-2005.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/5/4183/2005/acpd-5-4183-2005.pdf</fulltext_pdf>
	<start_page>4183</start_page>
	<end_page>4221</end_page>
	<publication_date>2005-06-28</publication_date>
	<article_title content_type="html">Characterization of ambient aerosols in Mexico City during the MCMA-2003 campaign with Aerosol Mass Spectrometry – Part II: overview of the results at the CENICA supersite and comparison to previous studies</article_title>
	<authors>
		<author numeration="1" affiliations="1,2">
			<name>D. Salcedo</name>
		</author>
		<author numeration="2" affiliations="2,3">
			<name>K. Dzepina</name>
		</author>
		<author numeration="3" affiliations="4">
			<name>T. B. Onasch</name>
		</author>
		<author numeration="4" affiliations="4">
			<name>M. R. Canagaratna</name>
		</author>
		<author numeration="5" affiliations="4">
			<name>J. T. Jayne</name>
		</author>
		<author numeration="6" affiliations="4">
			<name>D. R. Worsnop</name>
		</author>
		<author numeration="7" affiliations="5">
			<name>J S. Gaffney</name>
		</author>
		<author numeration="8" affiliations="5">
			<name>N. A. Marley</name>
		</author>
		<author numeration="9" affiliations="6">
			<name>K. S. Johnson</name>
		</author>
		<author numeration="10" affiliations="6,8">
			<name>B. Zuberi</name>
		</author>
		<author numeration="11" affiliations="6">
			<name>L. T. Molina</name>
		</author>
		<author numeration="12" affiliations="6">
			<name>M. J. Molina</name>
		</author>
		<author numeration="13" affiliations="7">
			<name>V. Shutthanandan</name>
		</author>
		<author numeration="14" affiliations="7">
			<name>Y. Xie</name>
		</author>
		<author numeration="15" affiliations="2,3">
			<name>J. L. Jimenez</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Centro de Investigaciones Qu&amp;#237;micas, Universidad Aut&amp;#243;noma del Estado de Morelos, Cuernavaca, Mexico</affiliation>
		<affiliation numeration="2" content_type="html">Cooperative Institute for Research in the Environmental Sciences (CIRES), University of Colorado at Boulder, Boulder, CO, USA</affiliation>
		<affiliation numeration="3" content_type="html">Department of Chemistry and Biochemistry, University of Colorado at Boulder, Boulder, CO, USA</affiliation>
		<affiliation numeration="4" content_type="html">Center for Aerosol and Cloud Chemistry, Aerodyne Research Inc., Billerica, MA, USA</affiliation>
		<affiliation numeration="5" content_type="html">Argonne National Laboratory, Argonne, IL, USA</affiliation>
		<affiliation numeration="6" content_type="html">Department of Earth, Atmospheric and Planetary Sciences and Department of Chemistry, Massachusetts Institute of Technology, Cambridge, MA, USA</affiliation>
		<affiliation numeration="7" content_type="html">William R. Wiley Environmental Molecular Sciences Laboratory, Pacific Northwest National Laboratory, Richland, WA, USA</affiliation>
		<affiliation numeration="8" content_type="html">now at: GEO2 Technologies, Woburn, MA, USA</affiliation>
	</affiliations>
	<abstract content_type="html">An Aerodyne Aerosol Mass Spectrometer (AMS) was deployed at the CENICA
Supersite during the Mexico City Metropolitan Area field study from 31 March&amp;ndash;4
May 2003. The AMS provides real time information on mass concentration
and composition of the non-refractory species in particulate matter less
than 1 &amp;micro;m (NR-PM&lt;sub&gt;1&lt;/sub&gt;) with high time and size-resolution.
Measurements of Black Carbon (BC) using an aethalometer, and estimated soil
concentrations from Proton-Induced X-Ray Emission (PIXE) analysis of
impactor substrates are also presented and combined with the AMS in order to
include refractory material and estimate the total PM&lt;sub&gt;2.5&lt;/sub&gt; mass
concentration at CENICA during this campaign. In Mexico City, the organic
fraction of the estimated PM&lt;sub&gt;2.5&lt;/sub&gt; at CENICA represents 54.6% of the
mass, with the rest consisting of inorganic compounds (mainly ammonium
nitrate and sulfate/ammonium salts), BC, and soil. Inorganic compounds
represent 27.5% of PM&lt;sub&gt;2.5&lt;/sub&gt;; BC mass concentration is about 11%;
while soil represents about 6.9%. The NR species and BC have diurnal
cycles that can be qualitatively interpreted as the interplay of direct
emissions, photochemical production in the atmosphere followed by
condensation and gas-to-particle partitioning, boundary layer dynamics,
and/or advection. Bi- and trimodal size distributions are observed for
the AMS species, with a small combustion (likely traffic) organic particle
mode and an accumulation mode that contains mainly organic and secondary
inorganic compounds. The AMS and BC mass concentrations, size distributions,
and diurnal cycles are found to be qualitatively similar to those from most
previous field measurements in Mexico City.</abstract>
	<references>
	</references>
</article>

