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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-9-18727-2009</article-id>
<title-group>
<article-title>Decadal trends in aerosol chemical composition at Barrow, AK: 1976–2008</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Quinn</surname>
<given-names>P. K.</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>Bates</surname>
<given-names>T. S.</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>Schulz</surname>
<given-names>K.</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>Shaw</surname>
<given-names>G. E.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>NOAA PMEL, 7600 Sand Point Way NE, Seattle, WA 98115, USA</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>University of Alaska, 903 Koyukuk Dr., Fairbanks, AK, 99775, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>10</day>
<month>09</month>
<year>2009</year>
</pub-date>
<volume>9</volume>
<issue>5</issue>
<fpage>18727</fpage>
<lpage>18743</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-discuss.net/9/18727/2009/acpd-9-18727-2009.html">This article is available from http://www.atmos-chem-phys-discuss.net/9/18727/2009/acpd-9-18727-2009.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys-discuss.net/9/18727/2009/acpd-9-18727-2009.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys-discuss.net/9/18727/2009/acpd-9-18727-2009.pdf</self-uri>
<abstract>
<p>Aerosol measurements at Barrow, AK during the past 30 years have identified
the long range transport of pollution associated with Arctic Haze as well as
ocean-derived aerosols of more local origin. Here, we focus on measurements
of aerosol chemical composition to assess 1) trends in Arctic Haze aerosol
and implications for source regions, 2) the interaction between
pollution-derived and ocean-derived aerosols and the resulting impacts on
the chemistry of the Arctic boundary layer, and 3) the response of aerosols
to a changing climate. Aerosol chemical composition measured at Barrow, AK
during the Arctic haze season is compared for the years 1976–1977 and
1997–2008. Based on these two data sets, concentrations of non-sea salt
(nss) sulfate (SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;=&lt;/sup&gt;) and non-crustal (nc) vanadium (V) have
decreased by about 60% over this 30 year period. Consistency in the
ratios of nss SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;=&lt;/sup&gt;/ncV and nc manganese (Mn)/ncV between the two
data sets indicates that, although emissions have decreased in the source
regions, the source regions have remained the same over this time period.
The measurements from 1997–2008 indicate that, during the haze season, the
nss SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;=&lt;/sup&gt; aerosol at Barrow is becoming less neutralized by
ammonium (NH&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;+&lt;/sup&gt;) yielding an increasing sea salt aerosol chloride
(Cl&lt;sup&gt;&amp;minus;&lt;/sup&gt;) deficit. The expected consequence is an increase in the release
of Cl atoms to the atmosphere and a change in the lifetime of volatile
organic compounds (VOCs) including methane. In addition, summertime
concentrations of biogenically-derived methanesulfonate (MSA&lt;sup&gt;&amp;minus;&lt;/sup&gt;) and nss
SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;=&lt;/sup&gt; are increasing at a rate of 12 and 8% per year,
respectively. Further research is required to assess the environmental
factors behind the increasing concentrations of biogenic aerosol.</p>
</abstract>
<counts><page-count count="17"/></counts>
</article-meta>
</front>
<body/>
<back>
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