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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-12-4165-2012</article-id>
<title-group>
<article-title>Atmospheric histories and growth trends of C&lt;sub&gt;4&lt;/sub&gt;F&lt;sub&gt;10&lt;/sub&gt;, C&lt;sub&gt;5&lt;/sub&gt;F&lt;sub&gt;12&lt;/sub&gt;, C&lt;sub&gt;6&lt;/sub&gt;F&lt;sub&gt;14&lt;/sub&gt;, C&lt;sub&gt;7&lt;/sub&gt;F&lt;sub&gt;16&lt;/sub&gt; and C&lt;sub&gt;8&lt;/sub&gt;F&lt;sub&gt;18&lt;/sub&gt;</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Ivy</surname>
<given-names>D. J.</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>Arnold</surname>
<given-names>T.</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>Harth</surname>
<given-names>C. 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>Steele</surname>
<given-names>L. P.</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>Mühle</surname>
<given-names>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>Rigby</surname>
<given-names>M.</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>Salameh</surname>
<given-names>P. K.</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>Leist</surname>
<given-names>M.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Krummel</surname>
<given-names>P. B.</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>Fraser</surname>
<given-names>P. J.</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>Weiss</surname>
<given-names>R. F.</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>Prinn</surname>
<given-names>R. 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>Center for Global Change Science, Massachusetts Institute of Technology, Cambridge, Massachusetts, USA</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Scripps Institution of Oceanography, Univ. of California San Diego, La Jolla, California, USA</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Centre for Australian Weather and Climate Research, CSIRO Marine and Atmospheric Research, Aspendale, Victoria, Australia</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>now at: Atmospheric Chemistry Research Group, University of Bristol, Bristol, UK</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>now at: Defence Science and Technology Organisation, Department of Defence, Melbourne, Victoria, Australia</addr-line>
</aff>
<pub-date pub-type="epub">
<day>03</day>
<month>02</month>
<year>2012</year>
</pub-date>
<volume>12</volume>
<issue>2</issue>
<fpage>4165</fpage>
<lpage>4184</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/12/4165/2012/acpd-12-4165-2012.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys-discuss.net/12/4165/2012/acpd-12-4165-2012.pdf</self-uri>
<abstract>
<p>The first atmospheric observations and trends are presented
      for the high molecular weight perfluorocarbons (PFCs):
      decafluorobutane (C&lt;sub&gt;4&lt;/sub&gt;F&lt;sub&gt;10&lt;/sub&gt;), dodecafluoropentane
      (C&lt;sub&gt;5&lt;/sub&gt;F&lt;sub&gt;12&lt;/sub&gt;), tetradecafluorohexane (C&lt;sub&gt;6&lt;/sub&gt;F&lt;sub&gt;14&lt;/sub&gt;),
      hexadecafluoroheptane (C&lt;sub&gt;7&lt;/sub&gt;F&lt;sub&gt;16&lt;/sub&gt;) and
      octadecafluorooctane (C&lt;sub&gt;8&lt;/sub&gt;F&lt;sub&gt;18&lt;/sub&gt;). Their atmospheric
      histories are based on measurements of 38 Northern Hemisphere
      and 46 Southern Hemisphere archived air samples collected
      between 1973 to 2011 using the Advanced Global Atmospheric
      Gases Experiment (AGAGE) &quot;Medusa&quot; preconcentration gas
      chromatography-mass spectrometry systems. A new calibration
      scale was prepared for each PFC, with estimated accuracies of
      6.8% for C&lt;sub&gt;4&lt;/sub&gt;F&lt;sub&gt;10&lt;/sub&gt;, 7.8% for
      C&lt;sub&gt;5&lt;/sub&gt;F&lt;sub&gt;12&lt;/sub&gt;, 4.0% for C&lt;sub&gt;6&lt;/sub&gt;F&lt;sub&gt;14&lt;/sub&gt;, 6.6%
      for C&lt;sub&gt;7&lt;/sub&gt;F&lt;sub&gt;16&lt;/sub&gt; and 7.9% for C&lt;sub&gt;8&lt;/sub&gt;F&lt;sub&gt;18&lt;/sub&gt;. Based
      on our observations the 2011 globally averaged dry air mole
      fractions of these heavy PFCs are: 0.18 parts-per-trillion
      (ppt, i.e., parts per 10&lt;sup&gt;12&lt;/sup&gt;) for C&lt;sub&gt;4&lt;/sub&gt;F&lt;sub&gt;10&lt;/sub&gt;, 0.12
      ppt for C&lt;sub&gt;5&lt;/sub&gt;F&lt;sub&gt;12&lt;/sub&gt;, 0.28 ppt for C&lt;sub&gt;6&lt;/sub&gt;F&lt;sub&gt;14&lt;/sub&gt;, 0.12
      ppt for C&lt;sub&gt;7&lt;/sub&gt;F&lt;sub&gt;16&lt;/sub&gt; and 0.09 ppt for
      C&lt;sub&gt;8&lt;/sub&gt;F&lt;sub&gt;18&lt;/sub&gt;. These atmospheric mole fractions combine to
      contribute to a global average radiative forcing of
      0.35 mW m&lt;sup&gt;−2&lt;/sup&gt;, which is 3.6% of the total PFC
      radiative forcing. The globally averaged mean atmospheric
      growth rates of these PFCs during 1973–2011 are 4.58 parts
      per quadrillion (ppq, i.e., parts per 10&lt;sup&gt;15&lt;/sup&gt;) per year (yr)
      for C&lt;sub&gt;4&lt;/sub&gt;F&lt;sub&gt;10&lt;/sub&gt;, 3.29 ppq yr&lt;sup&gt;−1&lt;/sup&gt; for
      C&lt;sub&gt;5&lt;/sub&gt;F&lt;sub&gt;12&lt;/sub&gt;, 7.50 ppq yr&lt;sup&gt;−1&lt;/sup&gt; for C&lt;sub&gt;6&lt;/sub&gt;F&lt;sub&gt;14&lt;/sub&gt;,
      3.19 ppq yr&lt;sup&gt;−1&lt;/sup&gt; for C&lt;sub&gt;7&lt;/sub&gt;F&lt;sub&gt;16&lt;/sub&gt; and
      2.51 ppq yr&lt;sup&gt;−1&lt;/sup&gt; for C&lt;sub&gt;8&lt;/sub&gt;F&lt;sub&gt;18&lt;/sub&gt;. The growth rates of
      the heavy perfluorocarbons were largest in the early 1990s for
      C&lt;sub&gt;4&lt;/sub&gt;F&lt;sub&gt;10&lt;/sub&gt; and C&lt;sub&gt;5&lt;/sub&gt;F&lt;sub&gt;12&lt;/sub&gt; and in the mid-to-late
      1990s for C&lt;sub&gt;6&lt;/sub&gt;F&lt;sub&gt;14&lt;/sub&gt;, C&lt;sub&gt;7&lt;/sub&gt;F&lt;sub&gt;16&lt;/sub&gt; and
      C&lt;sub&gt;8&lt;/sub&gt;F&lt;sub&gt;18&lt;/sub&gt;. The more recent slow down in the growth
      rates of the high molecular weight PFCs suggests that
      emissions are declining as compared to the 1980s and
      1990s. Nevertheless continued monitoring of these potent,
      extremely long-lived greenhouse gases is necessary to verify
      that global PFC emissions continue to decline.</p>
</abstract>
<counts><page-count count="20"/></counts>
</article-meta>
</front>
<body/>
<back>
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