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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-13-245-2013</article-id>
<title-group>
<article-title>Ice nuclei in marine air: biogenic particles or dust?</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Burrows</surname>
<given-names>S. M.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</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>Hoose</surname>
<given-names>C.</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>Pöschl</surname>
<given-names>U.</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>Lawrence</surname>
<given-names>M. G.</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-group><aff id="aff1">
<label>1</label>
<addr-line>Max Planck Institute for Chemistry, Mainz, Germany</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Institute for Meteorology and Climate Research &amp;ndash; Atmospheric Aerosol Research, Karlsruhe Institute of Technology, Karlsruhe, Germany</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>now at: Pacific Northwest National Laboratory, Richland, Washington, USA</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>now at: Institute for Advanced Sustainability Studies e.V., Potsdam, Germany</addr-line>
</aff>
<pub-date pub-type="epub">
<day>11</day>
<month>01</month>
<year>2013</year>
</pub-date>
<volume>13</volume>
<issue>1</issue>
<fpage>245</fpage>
<lpage>267</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/13/245/2013/acp-13-245-2013.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/13/245/2013/acp-13-245-2013.pdf</self-uri>
<abstract>
<p>Ice nuclei impact clouds, but their sources and
  distribution in the atmosphere are still not well known.
  Particularly little attention has been paid to IN sources in marine
  environments, although evidence from field studies suggests that IN
  populations in remote marine regions may be dominated by primary
  biogenic particles associated with sea spray.  In this exploratory
  model study, we aim to bring attention to this long-neglected topic
  and identify promising target regions for future field campaigns.
  We assess the likely global distribution of marine biogenic ice
  nuclei using a combination of historical observations, satellite
  data and model output.  By comparing simulated marine biogenic
  immersion IN distributions and dust immersion IN distributions, we
  predict strong regional differences in the importance of marine
  biogenic IN relative to dust IN.  Our analysis suggests that marine
  biogenic IN are most likely to play a dominant role in determining
  IN concentrations in near-surface-air over the Southern Ocean, so
  future field campaigns aimed at investigating marine biogenic IN
  should target that region.  Climate-related changes in the abundance
  and emission of biogenic marine IN could affect marine cloud
  properties, thereby introducing previously unconsidered feedbacks
  that influence the hydrological cycle and the Earth&apos;s energy
  balance.  Furthermore, marine biogenic IN may be an important aspect
  to consider in proposals for marine cloud brightening by artificial
  sea spray production.</p>
</abstract>
<counts><page-count count="23"/></counts>
</article-meta>
</front>
<body/>
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