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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>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acp-11-6773-2011</article-id>
<title-group>
<article-title>Aerosol flux measurements above a mixed forest at Borden, Ontario</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Gordon</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>Staebler</surname>
<given-names>R. 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>Liggio</surname>
<given-names>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>Vlasenko</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>Li</surname>
<given-names>S.-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>Hayden</surname>
<given-names>K.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Science and Technology Branch, Environment Canada, Toronto, Canada</addr-line>
</aff>
<pub-date pub-type="epub">
<day>18</day>
<month>07</month>
<year>2011</year>
</pub-date>
<volume>11</volume>
<issue>14</issue>
<fpage>6773</fpage>
<lpage>6786</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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<abstract>
<p>Aerosol fluxes were measured above a mixed forest by Eddy Covariance (EC)
with a Fast Mobility Particle Sizer (FMPS) at the Borden Forest Research
Station in Ontario, Canada between 13 July and 12 August 2009. Chemically
speciated flux measurements were made at a height of 29 m at the same
location between 19 July and 2 August, 2006 using a Quadrupole Aerosol Mass
Spectrometer (Q-AMS). The Q-AMS measured an average sulphate deposition
velocity of 0.3 mm s&lt;sup&gt;−1&lt;/sup&gt; and an average nitrate deposition velocity of
4.8 mm s&lt;sup&gt;−1&lt;/sup&gt;. The FMPS, mounted at a height of 33 m (approximately 10 m
above the canopy top) and housed in a temperature controlled enclosure,
measured size-resolved particle concentrations from 3 to 410 nm diameter at
a rate of 1 Hz. For the size range 18 &lt;  &lt;i&gt;D&lt;/i&gt; &lt; 452 nm, 60 % of fluxes were
upward. The exchange velocity was between −0.5 and 2.0 mm s&lt;sup&gt;−1&lt;/sup&gt;, with
median values near 0.5 mm s&lt;sup&gt;−1&lt;/sup&gt; for all sizes between 22 and 310 nm. The
size distribution of the apparent production rate of particles at 33 m
peaked at a diameter of 75 nm. Results indicate a decoupling of the above
and below canopy spaces, whereby particles are stored in the canopy space at
night, and are then diluted with cleaner air above during the day.</p>
</abstract>
<counts><page-count count="14"/></counts>
</article-meta>
</front>
<body/>
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