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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-12-9399-2012</article-id>
<title-group>
<article-title>Profiling of fine and coarse particle mass: case studies of Saharan dust and EyjafjallajÃ¶kull/GrimsvÃ¶tn volcanic  plumes</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Ansmann</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>Seifert</surname>
<given-names>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>Tesche</surname>
<given-names>M.</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>Wandinger</surname>
<given-names>U.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Leibniz Institute for Tropospheric Research, Leipzig, Germany</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Department of Applied Environmental Science,  Stockholm University, Stockholm, Sweden</addr-line>
</aff>
<pub-date pub-type="epub">
<day>17</day>
<month>10</month>
<year>2012</year>
</pub-date>
<volume>12</volume>
<issue>20</issue>
<fpage>9399</fpage>
<lpage>9415</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/12/9399/2012/acp-12-9399-2012.html">This article is available from http://www.atmos-chem-phys.net/12/9399/2012/acp-12-9399-2012.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/12/9399/2012/acp-12-9399-2012.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/12/9399/2012/acp-12-9399-2012.pdf</self-uri>
<abstract>
<p>The polarization lidar photometer networking (POLIPHON) method introduced to separate coarse-mode and fine-mode
particle properties of EyjafjallajÃ¶kull volcanic aerosols in 2010 is extended
to cover Saharan dust events as well. Furthermore, new volcanic dust
observations performed after the GrimsvÃ¶tn volcanic eruptions in 2011 are
presented. The retrieval of particle mass concentrations requires
mass-specific extinction coefficients. Therefore, a review of recently
published mass-specific extinction coefficients for Saharan dust and volcanic
dust is given. Case studies of four different scenarios corroborate the
applicability of the profiling technique: (a) Saharan dust outbreak to
central Europe, (b) Saharan dust plume mixed with biomass-burning smoke over
Cape Verde, and volcanic aerosol layers originating from (c) the
EyjafjallajÃ¶kull eruptions in 2010 and (d) the GrimsvÃ¶tn eruptions in
2011. Strong differences in the vertical aerosol layering, aerosol mixing,
and optical properties are observed for the different volcanic events.</p>
</abstract>
<counts><page-count count="17"/></counts>
</article-meta>
</front>
<body/>
<back>
<ref-list>
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