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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>GÃ¶ttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acp-10-4909-2010</article-id>
<title-group>
<article-title>Multi-year (2004â€“2008) record of nonmethane hydrocarbons and halocarbons in New England: seasonal variations and regional sources</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Russo</surname>
<given-names>R. 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>Zhou</surname>
<given-names>Y.</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>White</surname>
<given-names>M. L.</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>Mao</surname>
<given-names>H.</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>Talbot</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>Sive</surname>
<given-names>B. C.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Climate Change Research Center, Institute for the Study of Earth, Oceans, and Space, University of New Hampshire, Durham, NH 03824, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>27</day>
<month>05</month>
<year>2010</year>
</pub-date>
<volume>10</volume>
<issue>10</issue>
<fpage>4909</fpage>
<lpage>4929</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.net/10/4909/2010/acp-10-4909-2010.html">This article is available from http://www.atmos-chem-phys.net/10/4909/2010/acp-10-4909-2010.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/10/4909/2010/acp-10-4909-2010.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/10/4909/2010/acp-10-4909-2010.pdf</self-uri>
<abstract>
<p>Multi-year time series records of C&lt;sub&gt;2&lt;/sub&gt;-C&lt;sub&gt;6&lt;/sub&gt; alkanes, C&lt;sub&gt;2&lt;/sub&gt;-C&lt;sub&gt;4&lt;/sub&gt;
alkenes, ethyne, isoprene, C&lt;sub&gt;6&lt;/sub&gt;-C&lt;sub&gt;8&lt;/sub&gt; aromatics, trichloroethene
(C&lt;sub&gt;2&lt;/sub&gt;HCl&lt;sub&gt;3&lt;/sub&gt;), and tetrachloroethene (C&lt;sub&gt;2&lt;/sub&gt;Cl&lt;sub&gt;4&lt;/sub&gt;) from canister
samples collected during January 2004â€“February 2008 at the University of New
Hampshire (UNH) AIRMAP Observatory at Thompson Farm (TF) in Durham, NH are
presented. The objectives of this work are to identify the sources of
nonmethane hydrocarbons (NMHCs) and halocarbons observed at TF, characterize
the seasonal and interannual variability in ambient mixing ratios and
sources, and estimate regional emission rates of NMHCs. Analysis of
correlations and comparisons with emission ratios indicated that a
ubiquitous and persistent mix of emissions from several anthropogenic
sources is observed throughout the entire year. The highest C&lt;sub&gt;2&lt;/sub&gt;-C&lt;sub&gt;8&lt;/sub&gt;
anthropogenic NMHC mixing ratios were observed in mid to late winter.
Following the springtime minimums, the C&lt;sub&gt;3&lt;/sub&gt;-C&lt;sub&gt;6&lt;/sub&gt; alkanes,
C&lt;sub&gt;7&lt;/sub&gt;-C&lt;sub&gt;8&lt;/sub&gt; aromatics, and C&lt;sub&gt;2&lt;/sub&gt;HCl&lt;sub&gt;3&lt;/sub&gt; increased in early to mid
summer, presumably reflecting enhanced evaporative emissions. Mixing ratios
of C&lt;sub&gt;2&lt;/sub&gt;Cl&lt;sub&gt;4&lt;/sub&gt; and C&lt;sub&gt;2&lt;/sub&gt;HCl&lt;sub&gt;3&lt;/sub&gt; decreased by 0.7&amp;plusmn;0.2 and 0.3&amp;plusmn;0.05 pptv/year,
respectively, which is indicative of reduced usage
and emissions of these halogenated solvents. Emission rates of
C&lt;sub&gt;3&lt;/sub&gt;-C&lt;sub&gt;8&lt;/sub&gt; NMHCs were estimated to be 10&lt;sup&gt;9&lt;/sup&gt; to 10&lt;sup&gt;10&lt;/sup&gt; molecules cm&lt;sup&gt;âˆ’2&lt;/sup&gt; s&lt;sup&gt;âˆ’1&lt;/sup&gt;
in winter 2006. The emission rates extrapolated to the
state of New Hampshire and New England were ~2â€“60 Mg/day and ~12â€“430 Mg/day, respectively. Emission rates of benzene, toluene,
ethylbenzene, xylenes, and ethyne in the 2002 and 2005 EPA National
Emissions Inventories were within &amp;plusmn;50% of the TF emission rates.</p>
</abstract>
<counts><page-count count="21"/></counts>
</article-meta>
</front>
<body/>
<back>
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