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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ACPD</journal-id>
<journal-title-group>
<journal-title>Atmospheric Chemistry and Physics Discussions</journal-title>
<abbrev-journal-title abbrev-type="publisher">ACPD</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7375</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/acpd-12-5293-2012</article-id>
<title-group>
<article-title>Aerosol hygroscopicity at Ispra EMEP-GAW station</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Adam</surname>
<given-names>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>Putaud</surname>
<given-names>J. P.</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>Martins dos Santos</surname>
<given-names>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>Dell&apos;Acqua</surname>
<given-names>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>Gruening</surname>
<given-names>C.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>European Commission, Joint Research Centre, 21027, Ispra, Italy</addr-line>
</aff>
<pub-date pub-type="epub">
<day>17</day>
<month>02</month>
<year>2012</year>
</pub-date>
<volume>12</volume>
<issue>2</issue>
<fpage>5293</fpage>
<lpage>5340</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-discuss.net/12/5293/2012/acpd-12-5293-2012.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys-discuss.net/12/5293/2012/acpd-12-5293-2012.pdf</self-uri>
<abstract>
<p>This study focuses on the aerosol hygroscopic properties as determined from
ground-based measurements and Mie theory. Usually, aerosol ground-based
measurements are taken in dry conditions to ensure data consistency
within networks. The dependence of the various aerosol optical
characteristics (e.g. aerosol absorption, scattering, backscattering or
extinction coefficients) on relative humidity has therefore to be
established in order to determine their values in the atmosphere, where
relative humidity can reach high values.
&lt;br&gt;&lt;br&gt;
We calculated mean monthly diurnal values of the aerosol hygroscopic growth
factor at 90% relative humidity GF(90) based on measurements performed at
EMEP-GAW station of Ispra with a Hygroscopicity Tandem Differential Mobility
Analyzer over eight months in 2008 and 2009. Particle hygroscopicity
increases with particle dry diameter ranging from 35 to 165 nm for all
seasons. We observed a clear seasonal variation in GF(90) for particles larger
than 75 nm, and a diurnal cycle in spring and winter for all sizes. For
165 nm particles, GF(90) averages 1.32 &amp;plusmn; 0.06.
&lt;br&gt;&lt;br&gt;
The effect of the particle hygroscopic growth on the aerosol optical
properties (scattering, extinction, absorption and backscatter coefficients,
asymmetry parameter and backscatter faction) was computed using the Mie
theory, based on data obtained from a series of instruments running at our
station. We found median enhancement factors (defined as ratios between the
values of optical variables at 90% and 0% relative humidity) equal
to 1.1, 2.1, 1.7, and 1.8, for the aerosol absorption, scattering,
backscattering, and extinction coefficients, respectively. All except the
absorption enhancement factor show a strong correlation with the
hygroscopic growth factor. The enhancement factors observed at our site are
among the lowest observed across the world for the aerosol scattering
coefficient, and among the highest for the aerosol backscatter fraction.</p>
</abstract>
<counts><page-count count="48"/></counts>
</article-meta>
</front>
<body/>
<back>
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