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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-11-20713-2011</article-id>
<title-group>
<article-title>Characterization of the inter-annual, seasonal, and diurnal variations of condensation particle concentrations at Neumayer, Antarctica</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Weller</surname>
<given-names>R.</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>Minikin</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>Wagenbach</surname>
<given-names>D.</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>Dreiling</surname>
<given-names>V.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Alfred Wegener Institute for Polar and Marine Research, Am Handelshafen 12, 27570 Bremerhaven, Germany</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Deutsches Zentrum für Luft- und Raumfahrt (DLR), Institut für Physik der Atmosphäre, Oberpfaffenhofen, 82234 Weßling, Germany</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Institut für Umweltphysik, University Heidelberg, Im Neuenheimer Feld 229, 69120 Heidelberg, Germany</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Institut für Physik der Atmosphäre, Universität Mainz, 55099 Mainz, Germany</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>now at: Deutsches Zentrum für Luft- und Raumfahrt (DLR), Flugexperimente, Oberpfaffenhofen, 82234 Weßling, Germany</addr-line>
</aff>
<pub-date pub-type="epub">
<day>21</day>
<month>07</month>
<year>2011</year>
</pub-date>
<volume>11</volume>
<issue>7</issue>
<fpage>20713</fpage>
<lpage>20755</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/11/20713/2011/acpd-11-20713-2011.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys-discuss.net/11/20713/2011/acpd-11-20713-2011.pdf</self-uri>
<abstract>
<p>Continuous condensation particle (CP) observations were conducted from 1984
through 2009 at Neumayer Station under stringent contamination control.
During this period, the CP concentration (median 258 cm&lt;sup&gt;−3&lt;/sup&gt;) showed no
significant long term trend but exhibited a pronounced seasonality
characterized by a stepwise increase starting in September and reaching its
annual maximum of around 10&lt;sup&gt;3&lt;/sup&gt; cm&lt;sup&gt;−3&lt;/sup&gt; in March. Minimum values below
10&lt;sup&gt;2&lt;/sup&gt; cm&lt;sup&gt;−3&lt;/sup&gt; were observed during June/July. Dedicated time series
analyses in the time and frequency domain revealed no significant
correlations between inter-annual CP concentration variations and
atmospheric circulation indices like Southern Annular Mode (SAM) or Southern
Ocean Index (SOI). The impact of the Pinatubo volcanic eruption and strong
El Niño events did not affect CP concentrations. From thermodenuder
experiments we deduced that the portion of volatile (at 125 °C) and
semi-volatile (at 250 °C) particles which could be both associated with
biogenic sulfur aerosol, was maximum during austral summer, while during
winter non-volatile sea salt particles dominated. During September through
April we could frequently detect nucleation events which occurred
preferentially in the afternoon. Over the year, roughly 20 % of the
particles could be assigned to the nucleation mode between 3 nm and 7 nm
particle diameter.</p>
</abstract>
<counts><page-count count="43"/></counts>
</article-meta>
</front>
<body/>
<back>
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