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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-13-1579-2013</article-id>
<title-group>
<article-title>Characterization of long-term and seasonal variations of black carbon (BC) 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>Petzold</surname>
<given-names>A.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</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>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>König-Langlo</surname>
<given-names>G.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</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>now at: Forschungszentrum Jülich GmbH, Institut für Energie- und Klimaforschung IEK-8: Troposphäre, 52425 Jülich, Germany</addr-line>
</aff>
<pub-date pub-type="epub">
<day>08</day>
<month>02</month>
<year>2013</year>
</pub-date>
<volume>13</volume>
<issue>3</issue>
<fpage>1579</fpage>
<lpage>1590</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/13/1579/2013/acp-13-1579-2013.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/13/1579/2013/acp-13-1579-2013.pdf</self-uri>
<abstract>
<p>Continuous black carbon (BC) observations were conducted from 1999 through
2009 by an Aethalometer (AE10) and from 2006 through 2011 by a Multi-Angle
Absorption Photometer (MAAP) at Neumayer Station (NM) under stringent
contamination control. Considering the respective observation period, BC
concentrations measured by the MAAP were somewhat higher (median ±
standard deviation: 2.1 ± 2.0 ng m&lt;sup&gt;−3&lt;/sup&gt;) compared to the AE10 results
(1.6 ± 2.1 ng m&lt;sup&gt;−3&lt;/sup&gt;). Neither for the AE10 nor for the MAAP data set
a significant long-term trend could be detected. Consistently a pronounced
seasonality was observed with both instruments showing a primary annual
maximum between October and November and a minimum in April with a
maximum/minimum ratio of 4.5/1.6 = 3.8 and 2.7/0.64 = 4.2 for the MAAP
and AE10 data, respectively. Occasionally a secondary summer maximum in
January/February was visible. With the aim to assess the impact of BC on
optical properties of the aerosol at NM, we evaluated the BC data along with
particle scattering coefficients measured by an integrating nephelometer. We
found the mean single scattering albedo of &amp;omega;&lt;sub&gt;550&lt;/sub&gt; = 0.992 ± 0.0090
(median: 0.994) at a wavelength of 550 nm with a range
of values from 0.95 to 1.0.</p>
</abstract>
<counts><page-count count="12"/></counts>
</article-meta>
</front>
<body/>
<back>
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