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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-10-5749-2010</article-id>
<title-group>
<article-title>Size-dependent aerosol deposition velocities during BEARPEX&apos;07</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Vong</surname>
<given-names>R. J.</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>Vong</surname>
<given-names>I. J.</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>Vickers</surname>
<given-names>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>Covert</surname>
<given-names>D. S.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>College of Oceanic and Atmospheric Sciences, Oregon State University, Corvallis, OR 97331, USA</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Joint Institute for the Study of Atmospheres and Oceans, University of Washington, Seattle, WA 98195, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>30</day>
<month>06</month>
<year>2010</year>
</pub-date>
<volume>10</volume>
<issue>12</issue>
<fpage>5749</fpage>
<lpage>5758</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/10/5749/2010/acp-10-5749-2010.html">This article is available from http://www.atmos-chem-phys.net/10/5749/2010/acp-10-5749-2010.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/10/5749/2010/acp-10-5749-2010.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/10/5749/2010/acp-10-5749-2010.pdf</self-uri>
<abstract>
<p>Aerosol concentrations and 3-D winds were measured from 9 to 25 September 2007,
above a pine forest in California. The measurements were combined
using the eddy covariance (EC) technique to determine aerosol eddy fluxes as
a function of particle diameter within the accumulation mode size range
(0.25 μm&amp;le;&lt;i&gt;D&lt;/i&gt;&lt;sub&gt;p&lt;/sub&gt;&amp;le;1 μm here).
Measured heat and water vapor fluxes were utilized to correct the aerosol
eddy fluxes for aerosol hygroscopic growth. The hygroscopic growth
correction was necessary despite the low RH and relatively hygrophobic
nature of the particles. Uncertainties associated with particle counting
also were evaluated from the data. Aerosol deposition velocities
(&lt;i&gt;V&lt;/i&gt;&lt;sub&gt;d&lt;/sub&gt; = EC turbulent flux/mean particle concentration) during daytime were shown
to vary from −0.2 to −1.0 cm s&lt;sup&gt;−1&lt;/sup&gt;; the magnitude of particle &lt;i&gt;V&lt;/i&gt;&lt;sub&gt;d&lt;/sub&gt;
increases with friction velocity and particle diameter.</p>
</abstract>
<counts><page-count count="10"/></counts>
</article-meta>
</front>
<body/>
<back>
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