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<article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" article-type="research-article" dtd-version="3.0" xml:lang="en">
<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-11-4851-2011</article-id>
<title-group>
<article-title>The relationship between 0.25â€“2.5 Î¼m aerosol and CO&lt;sub&gt;2&lt;/sub&gt; emissions over a city</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Vogt</surname>
<given-names>M.</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>Nilsson</surname>
<given-names>E. D.</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>Ahlm</surname>
<given-names>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>MÃ¥rtensson</surname>
<given-names>E. M.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Johansson</surname>
<given-names>C.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Department of Applied Environmental Science (ITM), Stockholm University, 10691 Stockholm, Sweden</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>City of Stockholm Environment and Health Administration, P.O. Box 8136, 10420 Stockholm, Sweden</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Department of Earth Sciences, Uppsala University, 752 36 Uppsala, Sweden</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Scripps Institution of Oceanography, University of California, San Diego, La Jolla, CA, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>24</day>
<month>05</month>
<year>2011</year>
</pub-date>
<volume>11</volume>
<issue>10</issue>
<fpage>4851</fpage>
<lpage>4859</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.net/11/4851/2011/acp-11-4851-2011.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/11/4851/2011/acp-11-4851-2011.pdf</self-uri>
<abstract>
<p>Unlike exhaust emissions, non-exhaust traffic emissions are completely
unregulated and in addition, there are large uncertainties in the non-exhaust
emission factors required to estimate the emissions of these aerosols. This
study provides the first published results of direct measurements of size
resolved emission factors for particles in the size range
0.25â€“2.5 Î¼m using a new approach to derive aerosol emission
factors based on carbon dioxide (CO&lt;sub&gt;2&lt;/sub&gt;) emission fluxes. Aerosol fluxes
were measured over one year using the eddy covariance method at the top of a
105 m high communication tower in Stockholm, Sweden. Maximum CO&lt;sub&gt;2&lt;/sub&gt; and
particle fluxes were found when the wind direction coincided with the area of
densest traffic within the footprint area. Negative fluxes (uptake of
CO&lt;sub&gt;2&lt;/sub&gt; and deposition of particles) coincided with periods of sampling from
an urban forest area. The fluxes of CO&lt;sub&gt;2&lt;/sub&gt; were used to obtain emission
factors for particles by assuming that the CO&lt;sub&gt;2&lt;/sub&gt; fluxes could be directly
related to the amount of fuel burnt by vehicles in the footprint area. The
estimated emission factor for the fleet mix in the measurement area was, in
number 1.8 &amp;times; 10&lt;sup&gt;11&lt;/sup&gt; particle veh&lt;sup&gt;âˆ’1&lt;/sup&gt; km&lt;sup&gt;âˆ’1&lt;/sup&gt; (for
0.25â€“2.5 Î¼m size range). Assuming spherical particles of density
1600 kg m&lt;sup&gt;âˆ’3&lt;/sup&gt; this corresponds to 27.5 mg veh&lt;sup&gt;âˆ’1&lt;/sup&gt; km&lt;sup&gt;âˆ’1&lt;/sup&gt;. For
particles (0.8â€“2.5 Î¼m) the emission factors were
5.1 Ã— 10&lt;sup&gt;9&lt;/sup&gt; veh&lt;sup&gt;âˆ’1&lt;/sup&gt; km&lt;sup&gt;âˆ’1&lt;/sup&gt; for number and
11.5 mg veh&lt;sup&gt;âˆ’1&lt;/sup&gt; km&lt;sup&gt;âˆ’1&lt;/sup&gt; for mass. But a wind speed dependence was
noted for high wind speeds. Thus, for wind speeds larger than 9 m s&lt;sup&gt;âˆ’1&lt;/sup&gt;,
as measured in the tower at 105 m (&lt;i&gt;U&lt;/i&gt;&lt;sub&gt;105&lt;/sub&gt;), the emission factor for
particle number and mass was parameterised as: &lt;i&gt;E&lt;/i&gt;&lt;sub&gt;f&lt;/sub&gt; (Number, 0.8&amp;ndash;2.5 Î¼m) = (6.1 &amp;plusmn; 1.7)10&lt;sup&gt;9&lt;/sup&gt; &lt;i&gt;U&lt;/i&gt;&lt;sub&gt;105&lt;/sub&gt; &amp;minus;50 &amp;plusmn; 188
and &lt;i&gt;E&lt;/i&gt;&lt;sub&gt;f&lt;/sub&gt; (Mass, 0.8&amp;ndash;2.5 Î¼m) = (20 &amp;plusmn; 12) &lt;i&gt;U&lt;/i&gt;&lt;sub&gt;105&lt;/sub&gt; &amp;minus; 171 &amp;plusmn;122.</p>
</abstract>
<counts><page-count count="9"/></counts>
</article-meta>
</front>
<body/>
<back>
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