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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ACP</journal-id>
<journal-title-group>
<journal-title>Atmospheric Chemistry and Physics</journal-title>
<abbrev-journal-title abbrev-type="publisher">ACP</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7324</issn>
<publisher><publisher-name>Copernicus GmbH</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acp-7-1645-2007</article-id>
<title-group>
<article-title>Estimation of a &quot;radiatively correct&quot; black carbon specific absorption during the Mexico City Metropolitan Area (MCMA) 2003 field campaign</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Barnard</surname>
<given-names>J. C.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Kassianov</surname>
<given-names>E. I.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Ackerman</surname>
<given-names>T. P.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Johnson</surname>
<given-names>K.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Zuberi</surname>
<given-names>B.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Molina</surname>
<given-names>L. T.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Molina</surname>
<given-names>M. J.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Pacific Northwest National Laboratory, Richland, WA, USA</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Massachusetts Institute of Technology, Cambridge, MA, USA</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>now at: University of Washington, Seattle, WA, USA</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>now at: University of California, San Diego, CA, USA</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>now at: GEO&lt;sub&gt;2&lt;/sub&gt; Technologies, Woburn, MA, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>27</day>
<month>03</month>
<year>2007</year>
</pub-date>
<volume>7</volume>
<issue>6</issue>
<fpage>1645</fpage>
<lpage>1655</lpage>
<permissions>
<license xlink:type="simple">
<license-p>This is an open-access article ditributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.</license-p>
</license>
</permissions>
<self-uri xlink:href="http://www.atmos-chem-phys.net/7/1645/2007/acp-7-1645-2007.html">This article is available from http://www.atmos-chem-phys.net/7/1645/2007/acp-7-1645-2007.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/7/1645/2007/acp-7-1645-2007.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/7/1645/2007/acp-7-1645-2007.pdf</self-uri>
<abstract>
<p>During the Mexico City Metropolitan Area (MCMA) field campaign of 2003,
measurements of the shortwave radiation field allowed the inference of the
black carbon (BC) specific absorption, &amp;alpha;&lt;sub&gt;&amp;lambda;&lt;/sub&gt;, defined as the
monochromatic absorption cross section per unit mass (with units of
m&lt;sup&gt;2&lt;/sup&gt;/g). The averaged values of &amp;alpha;&lt;sub&gt;&amp;lambda;&lt;/sub&gt; derived from the method
here are either 8.9 m&lt;sup&gt;2&lt;/sup&gt;/g or 8.2 m&lt;sup&gt;2&lt;/sup&gt;/g at 500 nm, depending upon the
physical and optical parameters assumed for BC. These results are reasonably
consistent with those of Schuster et al. (2005), 9.5 m&lt;sup&gt;2&lt;/sup&gt;/g, and
Baumgartner et al. (2002), 7.0 m&lt;sup&gt;2&lt;/sup&gt;/g, both measured at 550 nm. The
&amp;alpha;&lt;sub&gt;&amp;lambda;&lt;/sub&gt; values reported in this paper should only be considered
effective, &quot;radiatively correct&quot; values because when used in radiative
transfer calculations the calculated irradiances match the measured
irradiances at 500 nm. The specific absorption so defined can assume a wide
range of values, depending upon: (1) the assumptions made prior to the
retrieval (e.g., shell/core aerosol configuration), and (2) values chosen
for BC density and refractive index. The range of possible values is large,
corresponding to a &quot;worst case&quot; uncertainty of about &amp;plusmn;70%,
assuming that all errors are additive and of the same sign so that no error
cancellation occurs.</p>
</abstract>
<counts><page-count count="11"/></counts>
</article-meta>
</front>
<body/>
<back>
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