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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-12-3627-2012</article-id>
<title-group>
<article-title>Night-time enhanced atmospheric ion concentrations in the marine boundary layer</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Kalivitis</surname>
<given-names>N.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff3">
<sup>3</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>Stavroulas</surname>
<given-names>I.</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>Bougiatioti</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>Kouvarakis</surname>
<given-names>G.</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>Gagné</surname>
<given-names>S.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
<xref ref-type="aff" rid="aff6">
<sup>6</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Manninen</surname>
<given-names>H. E.</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>Kulmala</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>Mihalopoulos</surname>
<given-names>N.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Environmental Chemical Processes Laboratory, Department of Chemistry, University of Crete, 71003, Heraklion, Greece</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Department of Physics, P.O. Box 64, 00014 University of Helsinki, Finland</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Department of Physical Geography and Quaternary Geology, Stockholm University, 10691 Stockholm, Sweden</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Navarino Environmental Observatory (NEO), Messinia, Greece</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>Department of Physics and Atmospheric Science, Dalhousie University, Halifax, B3H 3J5, Canada</addr-line>
</aff>
<aff id="aff6">
<label>6</label>
<addr-line>Environment Canada, Toronto, M3H 5T4, Canada</addr-line>
</aff>
<pub-date pub-type="epub">
<day>17</day>
<month>04</month>
<year>2012</year>
</pub-date>
<volume>12</volume>
<issue>8</issue>
<fpage>3627</fpage>
<lpage>3638</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/12/3627/2012/acp-12-3627-2012.html">This article is available from http://www.atmos-chem-phys.net/12/3627/2012/acp-12-3627-2012.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/12/3627/2012/acp-12-3627-2012.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/12/3627/2012/acp-12-3627-2012.pdf</self-uri>
<abstract>
<p>Measurements of atmospheric ions in the size range 0.8–42 nm were
conducted at the environmental research station of the University of Crete
at Finokalia from April 2008 to April 2009 in the frame of the EUCAARI
project. Both positive and negative atmospheric ions were found to have a
clear annual cycle, with minimum concentrations in summer. Their
concentrations were found to vary with the prevailing meteorology and the
abundance of aerosol particles in the atmosphere. High concentrations of
ions were observed during new particle formation events. There were 53
nucleation events recorded. It was found that under certain atmospheric
conditions enhanced ion concentrations can be observed during night.
Overall, 39 night-time events were observed, all of them observed for the
negatively charged particles while only 21 were observed for the positively
charged particles. Night-time enhanced ion concentrations were more frequent
during spring and autumn and no such events were recorded from July to
September. A strong anti-correlation was found between air ion
concentrations, especially at cluster sizes (1.25–1.66 nm), and
condensation and coagulation sinks. Enhanced ion concentrations at night
were found to be more frequent when air masses had traveled over the island
of Crete, indicating possible association with local biogenic sources.</p>
</abstract>
<counts><page-count count="12"/></counts>
</article-meta>
</front>
<body/>
<back>
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