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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>5</volume_number>
		<issue_number>3</issue_number>
		<publication_year>2005</publication_year>
	</journal>
	<doi>10.5194/acpd-5-4083-2005</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/5/4083/2005/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/5/4083/2005/acpd-5-4083-2005.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/5/4083/2005/acpd-5-4083-2005.pdf</fulltext_pdf>
	<start_page>4083</start_page>
	<end_page>4113</end_page>
	<publication_date>2005-06-23</publication_date>
	<article_title content_type="html">Measurements of Black Carbon Specific Absorption in the Mexico City Metropolitan Area during the MCMA 2003 Field Campaign</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>J. C. Barnard</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>E. I. Kassianov</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>T. P. Ackerman</name>
		</author>
		<author numeration="4" affiliations="2">
			<name>S. Frey</name>
		</author>
		<author numeration="5" affiliations="2">
			<name>K. Johnson</name>
		</author>
		<author numeration="6" affiliations="2,4">
			<name>B. Zuberi</name>
		</author>
		<author numeration="7" affiliations="2">
			<name>L. T. Molina</name>
		</author>
		<author numeration="8" affiliations="2">
			<name>M. J. Molina</name>
		</author>
		<author numeration="9" affiliations="3">
			<name>J. S. Gaffney</name>
		</author>
		<author numeration="10" affiliations="3">
			<name>N. A. Marley</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Pacific Northwest National Laboratory, Richland, Washington, USA</affiliation>
		<affiliation numeration="2" content_type="html">Massachusetts Institute of Technology, Cambridge, Massachusetts, USA</affiliation>
		<affiliation numeration="3" content_type="html">Argonne National Laboratory, Argonne, Illinois, USA</affiliation>
		<affiliation numeration="4" content_type="html">now at: GEO2 Technologies, Weston, Massachusetts, USA</affiliation>
	</affiliations>
	<abstract content_type="html">During the Mexico City Metropolitan Area (MCMA) field campaign of 2003,
measurements of the shortwave radiation field, lidar backscatter, and
atmospheric concentrations of black carbon (BC) permitted the inference of
the BC carbon specific absorption, &amp;alpha;&lt;sub&gt;&amp;lambda;&lt;/sub&gt;, defined as the absorption
cross section per unit mass (with units of m&lt;sup&gt;2&lt;/sup&gt;/g). This diverse set of
measurements allowed us to determine &amp;alpha;&lt;sub&gt;&amp;lambda;&lt;/sub&gt; in two ways. These
methods &amp;ndash; labeled I and II &amp;ndash; are distinguished from one another in the
manner that the columnar concentration of BC (with units of 
mg/m&lt;sup&gt;2&lt;/sup&gt; is
determined. This concentration is found by using either surface measurements
of BC concentration and lidar estimates of aerosol mixing heights, or a more
rigorous method that relies on the columnar aerosol size distribution. The
averaged values of &amp;alpha;&lt;sub&gt;&amp;lambda;&lt;/sub&gt; derived from these methods agree to about
20%, although we expect that the values obtained from method&amp;nbsp;I are
underestimated. These results, along with those of Schuster et al.&amp;nbsp;(2005),
suggest that in the MCMA, &amp;alpha;&lt;sub&gt;&amp;lambda;&lt;/sub&gt; is in a range of 8 to 
10 m&lt;sup&gt;2&lt;/sup&gt;/g
at a wavelength of 550 nm. This range is somewhat lower than the commonly
accepted value of 10 m&lt;sup&gt;2&lt;/sup&gt;/g for a wavelength of 550 nm, but is consistent
with the calculations of Fuller et al.&amp;nbsp;(1999), who suggest that this value
is too high.</abstract>
	<references>
	</references>
</article>

