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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>
<abbrev-journal-title abbrev-type="nlm-ta">Atmos. Chem. Phys.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7324</issn>
<publisher><publisher-name>Copernicus Publications</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acp-8-7193-2008</article-id>
<title-group>
<article-title>Measurements of size-resolved hygroscopicity in the California coastal zone</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Hegg</surname>
<given-names>D. A.</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>Covert</surname>
<given-names>D. 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>Jonsson</surname>
<given-names>H. H.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Department of Atmospheric Sciences, University of Washington, Seattle, WA, USA</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Meteorology Department, Naval Post Graduate School, Monterey, CA, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>09</day>
<month>12</month>
<year>2008</year>
</pub-date>
<volume>8</volume>
<issue>23</issue>
<fpage>7193</fpage>
<lpage>7203</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2008 D. A. Hegg et al.</copyright-statement>
<copyright-year>2008</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 3.0 Unported License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by/3.0/">https://creativecommons.org/licenses/by/3.0/</ext-link></license-p>
</license>
</permissions>
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<abstract>
<p>Aircraft-based measurements of aerosol hygroscopicity, both in the form of
size-resolved, diameter growth factors and in the dependence of particle
light scattering on relative humidity, are presented for the marine boundary
layer of the southern California coastal zone. The chemical composition of
the aerosol is collated with the hygroscopicity data, both to examine the
mechanism for the increase in aerosol hygroscopicity with altitude and as
input for receptor type modeling. The data suggest an increase in aerosol
hygroscopicity with altitude, possibly associated with oxidation of organic
films. The receptor modeling suggests three distinct aerosol types/sources
for this venue: marine, biomass burning and pollution. Model output is used
in regression analyses to derive a prognostic mixing rule for the
hygroscopicity of aerosol with these three sources. The mixing rule
demonstrated substantial prognostic power for submicron hygroscopicity but
essentially none for supermicron.</p>
</abstract>
<counts><page-count count="11"/></counts>
</article-meta>
</front>
<body/>
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