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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-12-9451-2012</article-id>
<title-group>
<article-title>Overview of aerosol properties associated with air masses sampled by the ATR-42 during the EUCAARI campaign (2008)</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Crumeyrolle</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>Schwarzenboeck</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>Sellegri</surname>
<given-names>K.</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>Burkhart</surname>
<given-names>J. F.</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>Stohl</surname>
<given-names>A.</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>Gomes</surname>
<given-names>L.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Quennehen</surname>
<given-names>B.</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>Roberts</surname>
<given-names>G.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Weigel</surname>
<given-names>R.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</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>Roger</surname>
<given-names>J. C.</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>Villani</surname>
<given-names>P.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</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>Pichon</surname>
<given-names>J. 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>Bourrianne</surname>
<given-names>T.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Laj</surname>
<given-names>P.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Laboratoire de Météorologie Physique, CNRS, Université  Blaise Pascal, UMR6016, Clermont-Ferrand, France</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Norwegian  Institute for Air Research, Kjeller, Norway</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Centre National de  Recherches Météorologiques, Météo-France, Toulouse, France</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Institute for Physics of the Atmosphere, Johannes Gutenberg  University, Mainz, Germany</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>Laboratoire de Glaciologie et  Géophysique de l&apos;Environnement, Université de Grenoble, CNRS, Grenoble,  France</addr-line>
</aff>
<pub-date pub-type="epub">
<day>12</day>
<month>04</month>
<year>2012</year>
</pub-date>
<volume>12</volume>
<issue>4</issue>
<fpage>9451</fpage>
<lpage>9490</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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<abstract>
<p>Within the frame of the European Aerosol Cloud Climate and Air Quality Interactions
  (EUCAARI) project the Météo-France aircraft ATR-42 performed 22 research flights,
  over central Europe and the North Sea during the intensive observation period in
  May 2008. For the campaign, the ATR-42 was equipped in order to study aerosol
  physical, chemical and optical properties, as well as cloud microphysics. During
   the campaign, continental air masses from Eastern and Western Europe were
   encountered, along with polar and Scandinavian air masses. For the 22 research
    flights, retroplume analyses along the flight tracks were performed with
    FLEXPART in order to classify air masses into five sectors of origin which
     allows for a qualitative evaluation of emission influence on the respective air parcel.
&lt;br&gt;&lt;/br&gt;
In the polluted boundary layer (BL), typical concentrations of particles with diameters
 larger than 10 nm (N&lt;sub&gt;10&lt;/sub&gt;) are of the order of 5000–6000 cm&lt;sup&gt;−3&lt;/sup&gt;, whereas N&lt;sub&gt;10&lt;/sub&gt;
  concentrations of clean air masses were lower than 1300 cm&lt;sup&gt;−3&lt;/sup&gt;. The detection of the
   largest particle number concentrations occurred in air masses coming from Polar and
   Scandinavian regions for which an elevated number of nucleation mode (25–28 nm)
   particles was observed and attributed to new particle formation over open sea. In
   the free troposphere (FT), typical observed N&lt;sub&gt;10&lt;/sub&gt; are of the order of
   900 cm&lt;sup&gt;−3&lt;/sup&gt; in polluted air masses and 400–600 cm&lt;sup&gt;−3&lt;/sup&gt; in clean air
   masses, respectively. In both layers, the chemical composition of submicron aerosol
    particles is dominated by organic matter and nitrate in polluted air masses,
    while, sulphate and ammonium followed by organics dominate the submicron
    aerosols in clean air masses. The highest CCN/CN ratios were observed within
     the polar air masses while the CCN concentration values are the highest within the polluted air masses.
&lt;br&gt;&lt;/br&gt;
Within the five air mass sectors defined and the two layers (BL and FT), observations have been
 distinguished into anticyclonic (first half of May 2008) and cyclonic conditions (second half of May 2008).
  Strong relationships between meteorological conditions  and physical, chemical as well as optical properties are found.</p>
</abstract>
<counts><page-count count="40"/></counts>
</article-meta>
</front>
<body/>
<back>
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