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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>GÃ¶ttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acp-11-12369-2011</article-id>
<title-group>
<article-title>Aerosol hygroscopicity and CCN activation kinetics in a boreal forest environment during the 2007 EUCAARI campaign</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Cerully</surname>
<given-names>K. M.</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>Raatikainen</surname>
<given-names>T.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</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>Lance</surname>
<given-names>S.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</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>Tkacik</surname>
<given-names>D.</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>Tiitta</surname>
<given-names>P.</given-names>
</name>
<xref ref-type="aff" rid="aff7">
<sup>7</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>PetÃ¤jÃ¤</surname>
<given-names>T.</given-names>
</name>
<xref ref-type="aff" rid="aff9">
<sup>9</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Ehn</surname>
<given-names>M.</given-names>
</name>
<xref ref-type="aff" rid="aff9">
<sup>9</sup>
</xref>
<xref ref-type="aff" rid="aff13">
<sup>13</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Kulmala</surname>
<given-names>M.</given-names>
</name>
<xref ref-type="aff" rid="aff9">
<sup>9</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Worsnop</surname>
<given-names>D. R.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
<xref ref-type="aff" rid="aff7">
<sup>7</sup>
</xref>
<xref ref-type="aff" rid="aff9">
<sup>9</sup>
</xref>
<xref ref-type="aff" rid="aff10">
<sup>10</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Laaksonen</surname>
<given-names>A.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</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>Smith</surname>
<given-names>J. N.</given-names>
</name>
<xref ref-type="aff" rid="aff7">
<sup>7</sup>
</xref>
<xref ref-type="aff" rid="aff11">
<sup>11</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Nenes</surname>
<given-names>A.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff12">
<sup>12</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>School of Chemical and Biomolecular Engineering, Georgia Institute of Technology, Atlanta, GA, USA</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>School of Earth and Atmospheric Science, Georgia Institute of Technology, Atlanta, GA, USA</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Finnish Meteorological Institute, Helsinki, Finland</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, CO, USA</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>Earth System Research Laboratory, National Oceanic and Atmospheric Administration, Boulder, CO, USA</addr-line>
</aff>
<aff id="aff6">
<label>6</label>
<addr-line>Center for Atmospheric Particle Studies, Carnegie Mellon University, Pittsburgh, PA, USA</addr-line>
</aff>
<aff id="aff7">
<label>7</label>
<addr-line>Department of Applied Physics, University of Eastern Finland, Kuopio, Finland</addr-line>
</aff>
<aff id="aff8">
<label>8</label>
<addr-line>Atmospheric Chemistry Research Group, North-West University, Potchefstroom, South Africa</addr-line>
</aff>
<aff id="aff9">
<label>9</label>
<addr-line>Department of Physics, University of Helsinki, Helsinki, Finland</addr-line>
</aff>
<aff id="aff10">
<label>10</label>
<addr-line>Aerodyne Research Incorporated, Billerica, MA, USA</addr-line>
</aff>
<aff id="aff11">
<label>11</label>
<addr-line>National Center for Atmospheric Research, Boulder, CO, USA</addr-line>
</aff>
<aff id="aff12">
<label>12</label>
<addr-line>Institute of Chemical Engineering and High-Temperature Chemical Processes, Foundation for Research and Technology Hellas, Patras, Greece</addr-line>
</aff>
<aff id="aff13">
<label>13</label>
<addr-line>currently at: Institute for Energy and Climate Research, Forschungszentrum JÃ¼lich, JÃ¼lich, Germany</addr-line>
</aff>
<pub-date pub-type="epub">
<day>09</day>
<month>12</month>
<year>2011</year>
</pub-date>
<volume>11</volume>
<issue>23</issue>
<fpage>12369</fpage>
<lpage>12386</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>
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<self-uri xlink:href="http://www.atmos-chem-phys.net/11/12369/2011/acp-11-12369-2011.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/11/12369/2011/acp-11-12369-2011.pdf</self-uri>
<abstract>
<p>Measurements of size-resolved cloud condensation nuclei (CCN) concentrations,
subsaturated hygroscopic growth, size distribution, and chemical composition
were collected from March through May, 2007, in the remote Boreal forests of
HyytiÃ¤lÃ¤, Finland, as part of the European Integrated project on
Aerosol Cloud Climate and Air Quality Interactions (EUCAARI) campaign.
Hygroscopicity parameter, &lt;i&gt;&amp;kappa;&lt;/i&gt;, distributions were derived
independently from Continuous Flow-Streamwise Thermal Gradient CCN Chamber
(CFSTGC) and Hygroscopicity Tandem Differential Mobility Analyzer (HTDMA)
measurements. CFSTGC-derived &lt;i&gt;&amp;kappa;&lt;/i&gt; values for 40, 60, and 80 nm
particles range mostly between 0.10 and 0.40 with an average characteristic
of highly oxidized organics of 0.20 Â± 0.10, indicating that organics
play a dominant role for this environment. HTDMA-derived &lt;i&gt;&amp;kappa;&lt;/i&gt; were
generally 30% lower. Diurnal trends of &lt;i&gt;&amp;kappa;&lt;/i&gt; show a minimum at
sunrise and a maximum in the late afternoon; this trend covaries with
inorganic mass fraction and the &lt;i&gt;m/z&lt;/i&gt; 44 organic mass fraction given
by a quadrupole aerosol mass spectrometer, further illustrating the
importance of organics in aerosol hygroscopicity. The chemical dispersion
inferred from the observed &lt;i&gt;&amp;kappa;&lt;/i&gt; distributions indicates that while 60
and 80 nm dispersion increases around midday, 40 nm dispersion remains
constant. Additionally, 80 nm particles show a markedly higher level of
chemical dispersion than both 40 and 60 nm particles. An analysis of droplet
activation kinetics for the sizes considered indicates that most of the CCN
activate as rapidly as (NH&lt;sub&gt;4&lt;/sub&gt;)&lt;sub&gt;2&lt;/sub&gt;SO&lt;sub&gt;4&lt;/sub&gt; calibration aerosol.</p>
</abstract>
<counts><page-count count="18"/></counts>
</article-meta>
</front>
<body/>
<back>
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