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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-11-5435-2011</article-id>
<title-group>
<article-title>Transport of anthropogenic emissions during ARCTAS-A: a climatology and regional case studies</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Harrigan</surname>
<given-names>D. L.</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 contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Fuelberg</surname>
<given-names>H. E.</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>Simpson</surname>
<given-names>I. J.</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>Blake</surname>
<given-names>D. R.</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>Carmichael</surname>
<given-names>G. R.</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>Diskin</surname>
<given-names>G. S.</given-names>
</name>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Department of Meteorology, Florida State University, Tallahassee, FL, USA</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Department of Chemistry, University of California, Irvine, CA, USA</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Center for Global and Regional Environmental Research, University of  Iowa, Iowa City, IA, USA</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>National Oceanic and Atmospheric Administration, National Weather  Service, Tallahassee, FL, USA</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>NASA Langley Research Center, Hampton, VA, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>15</day>
<month>02</month>
<year>2011</year>
</pub-date>
<volume>11</volume>
<issue>2</issue>
<fpage>5435</fpage>
<lpage>5491</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/11/5435/2011/acpd-11-5435-2011.html">This article is available from http://www.atmos-chem-phys-discuss.net/11/5435/2011/acpd-11-5435-2011.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys-discuss.net/11/5435/2011/acpd-11-5435-2011.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys-discuss.net/11/5435/2011/acpd-11-5435-2011.pdf</self-uri>
<abstract>
<p>The National Aeronautics and Space Administration (NASA) conducted the
      Arctic Research of the Composition of the Troposphere from Aircraft
      and Satellites (ARCTAS) mission during 2008 as a part of the
      International Polar Year (IPY). The purpose of ARCTAS was to study the
      factors responsible for changes in the Arctic&apos;s atmospheric
      composition and climate. A major emphasis was to investigate Arctic
      haze, which is most pronounced during winter and early spring. This
      study focuses on the spring phase of ARCTAS (ARCTAS-A) that was based
      in Alaska during April 2008. Although anthropogenic emissions
      historically have been associated with Arctic haze, biomass burning
      dominated the ARCTAS-A period and has been the focus of many ARCTAS
      related studies.
&lt;br&gt;&lt;/br&gt;
      This study determines the common pathways for anthropogenic emissions
      during ARCTAS-A. Trajectories (air parcels) are released each day from
      three historically significant regions of anthropogenic emissions
      (Asia, North America, and Europe). These fifteen day forward
      trajectories are calculated using data from the Weather Research and
      Forecasting (WRF) model at 45 km horizontal resolution. The
      trajectories then are examined to determine: origins of emissions that
      reach the Arctic (defined as north of 70° N) within fifteen
      days, pathways of the emissions reaching the Arctic, Arctic entry
      locations, and altitudes at which the trajectories enter the
      Arctic. These results serve as regional &quot;climatologies&quot; for the
      ARCTAS-A period.
&lt;br&gt;&lt;/br&gt;
      Three cases during the ARCTAS-A period (one for each of the regions
      above) are examined using backward trajectories and chemical
      fingerprinting based on in situ data sampled from the NASA DC-8. The
      fingerprinting utilizes volatile organic compounds that represent pure
      anthropogenic tracers, Asian anthropogenic pollution, incomplete
      combustion, and natural gas emissions. We determine flight legs
      containing anthropogenic emissions and the pathways travelled by these
      emissions. Results show that the DC-8 sampled anthropogenic emissions
      from Asia, North America, and Europe during the spring phase of
      ARCTAS. The pathways travelled by these emissions agree with our
      derived &quot;climatologies&quot; and previous studies of Arctic
      transport. Meteorological analysis and trajectory calculations
      indicate that middle latitude cyclones and their associated warm
      conveyor belts play an important role in lofting the surface based
      emissions to their sampling altitude in all three cases.</p>
</abstract>
<counts><page-count count="57"/></counts>
</article-meta>
</front>
<body/>
<back>
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