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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-9-6727-2009</article-id>
<title-group>
<article-title>Aerosol optical properties relevant to regional remote sensing of CCN activity and links to their organic mass fraction: airborne observations over Central Mexico and the US West Coast during MILAGRO/INTEX-B</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Shinozuka</surname>
<given-names>Y.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff7">
<sup>7</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Clarke</surname>
<given-names>A. D.</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>DeCarlo</surname>
<given-names>P. F.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
<xref ref-type="aff" rid="aff8">
<sup>8</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Jimenez</surname>
<given-names>J. L.</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>Dunlea</surname>
<given-names>E. J.</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>Roberts</surname>
<given-names>G. C.</given-names>
</name>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Tomlinson</surname>
<given-names>J. M.</given-names>
</name>
<xref ref-type="aff" rid="aff6">
<sup>6</sup>
</xref>
<xref ref-type="aff" rid="aff9">
<sup>9</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Collins</surname>
<given-names>D. R.</given-names>
</name>
<xref ref-type="aff" rid="aff6">
<sup>6</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Howell</surname>
<given-names>S. G.</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>Kapustin</surname>
<given-names>V. N.</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>McNaughton</surname>
<given-names>C. S.</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>Zhou</surname>
<given-names>J.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>School of Ocean and Earth Science and Technology, University of Hawaii, Honolulu, HI, USA</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Cooperative Institute for Research in the Environmental Sciences, University of Colorado, Boulder, CO, USA</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Dept. of Atmospheric and Oceanic Sciences, University of Colorado, Boulder, CO, USA</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Dept. of Chemistry and Biochemistry, University of Colorado, Boulder, CO, USA</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>Center for Atmospheric Sciences, Scripps Institution of Oceanography, La Jolla, CA, USA</addr-line>
</aff>
<aff id="aff6">
<label>6</label>
<addr-line>Department of Atmospheric Sciences, Texas A&amp;M University, College Station, TX, USA</addr-line>
</aff>
<aff id="aff7">
<label>7</label>
<addr-line>now at: NASA Postdoctoral Program, NASA Ames Research Center, MS 245-5, Moffett Field, CA, USA</addr-line>
</aff>
<aff id="aff8">
<label>8</label>
<addr-line>now at: Paul Scherrer Institut, 5232 Villigen-PSI, Switzerland</addr-line>
</aff>
<aff id="aff9">
<label>9</label>
<addr-line>now at: Pacific Northwest National Laboratory, Richland, WA, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>17</day>
<month>09</month>
<year>2009</year>
</pub-date>
<volume>9</volume>
<issue>18</issue>
<fpage>6727</fpage>
<lpage>6742</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/9/6727/2009/acp-9-6727-2009.html">This article is available from http://www.atmos-chem-phys.net/9/6727/2009/acp-9-6727-2009.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/9/6727/2009/acp-9-6727-2009.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/9/6727/2009/acp-9-6727-2009.pdf</self-uri>
<abstract>
<p>Remote sensing of cloud condensation nuclei (CCN) would help evaluate the
indirect effects of tropospheric aerosols on clouds and climate. To assess
its feasibility, we examined relationships of submicron aerosol composition
to CCN activity and optical properties observed during the MILAGRO/INTEX-B
aircraft campaigns. An indicator of CCN activity, κ, was calculated from
hygroscopicity measured under saturation. κ for dry 100 nm particles
decreased with increasing organic fraction of non-refractory mass of
submicron particles (OMF) as 0.34–0.20&amp;times;OMF over Central Mexico and
0.47–0.43&amp;times;OMF over the US West Coast. These fits represent the critical dry
diameter, centered near 100 nm for 0.2% supersaturation but varied as
&amp;kappa;&lt;sup&gt;(&amp;minus;1/3)&lt;/sup&gt;, within measurement uncertainty (~20%). The decreasing
trends of CCN activity with the organic content, evident also in our direct
CCN counts, were consistent with previous ground and laboratory observations
of highly organic particles. The wider range of OMF, 0–0.8, for our
research areas means that aerosol composition will be more critical for
estimation of CCN concentration than at the fixed sites previously studied.
Furthermore, the wavelength dependence of extinction was anti-correlated
with OMF as &amp;minus;0.70&amp;times;OMF+2.0 for Central Mexico&apos;s urban and industrial
pollution air masses, for unclear reasons. The Angstrom exponent of
absorption increased with OMF, more rapidly under higher single scattering
albedo, as expected for the interplay between soot and colored weak
absorbers (some organic species and dust). Because remote sensing products
currently use the wavelength dependence of extinction albeit in the column
integral form and may potentially include that of absorption, these regional
spectral dependencies are expected to facilitate retrievals of aerosol bulk
chemical composition and CCN activity over Central Mexico.</p>
</abstract>
<counts><page-count count="16"/></counts>
</article-meta>
</front>
<body/>
<back>
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