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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-9-271-2009</article-id>
<title-group>
<article-title>Emissions of volatile organic compounds inferred from airborne flux measurements over a megacity</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Karl</surname>
<given-names>T.</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>Apel</surname>
<given-names>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>Hodzic</surname>
<given-names>A.</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>Riemer</surname>
<given-names>D. D.</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="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Wiedinmyer</surname>
<given-names>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>National Center for Atmospheric Research, Boulder, CO, USA</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>University of Miami, Miami, FL, USA</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>University of California, Irvine, CA, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>14</day>
<month>01</month>
<year>2009</year>
</pub-date>
<volume>9</volume>
<issue>1</issue>
<fpage>271</fpage>
<lpage>285</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/9/271/2009/acp-9-271-2009.html">This article is available from http://www.atmos-chem-phys.net/9/271/2009/acp-9-271-2009.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/9/271/2009/acp-9-271-2009.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/9/271/2009/acp-9-271-2009.pdf</self-uri>
<abstract>
<p>Toluene and benzene are used for assessing the ability to measure
disjunct eddy covariance (DEC) fluxes of Volatile Organic Compounds (VOC)
using Proton Transfer Reaction Mass Spectrometry (PTR-MS) on aircraft.
Statistically significant correlation between vertical wind speed and mixing
ratios suggests that airborne VOC eddy covariance (EC) flux measurements
using PTR-MS are feasible. City-median midday toluene and benzene fluxes are
calculated to be on the order of 14.1&amp;plusmn;4.0 mg/m&lt;sup&gt;2&lt;/sup&gt;/h and 4.7&amp;plusmn;2.3 mg/m&lt;sup&gt;2&lt;/sup&gt;/h,
respectively. For comparison the adjusted CAM2004 emission
inventory estimates toluene fluxes of 10 mg/m&lt;sup&gt;2&lt;/sup&gt;/h along the footprint of
the flight-track. Wavelet analysis of instantaneous toluene and benzene
measurements during city overpasses is tested as a tool to assess surface
emission heterogeneity. High toluene to benzene flux ratios above an
industrial district (e.g. 10â€“15 g/g) including the International airport
(e.g. 3â€“5 g/g) and a mean flux (concentration) ratio of 3.2&amp;plusmn;0.5 g/g
(3.9&amp;plusmn;0.3 g/g) across Mexico City indicate that evaporative fuel and
industrial emissions play an important role for the prevalence of aromatic
compounds. Based on a tracer model, which was constrained by BTEX (BTEXâ€“
Benzene/Toluene/Ethylbenzene/m, p, o-Xylenes) compound
concentration ratios, the fuel marker methyl-tertiary-butyl-ether (MTBE) and
the biomass burning marker acetonitrile (CH&lt;sub&gt;3&lt;/sub&gt;CN), we show that a
combination of industrial, evaporative fuel, and exhaust emissions account
for &gt;87% of all BTEX sources. Our observations suggest that biomass
burning emissions play a minor role for the abundance of BTEX compounds in
the MCMA (2â€“13%).</p>
</abstract>
<counts><page-count count="15"/></counts>
</article-meta>
</front>
<body/>
<back>
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