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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-10-20303-2010</article-id>
<title-group>
<article-title>A subsiding regional forest fire aerosol layer at Whistler, BC: implications for interpretation of mountaintop chemistry observations</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Mc Kendry</surname>
<given-names>I. G.</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>Gallagher</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>Campuzano Jost</surname>
<given-names>P.</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>Bertram</surname>
<given-names>A.</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>Strawbridge</surname>
<given-names>K.</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>Leaitch</surname>
<given-names>R.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Macdonald</surname>
<given-names>A. M.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Department of Geography, The University of British Columbia, Vancouver, Canada</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Department of Chemistry, The University of British Columbia, Vancouver, Canada</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Centre for Atmospheric Research Experiments, Environment Canada, Egbert, Canada</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Science and Technology Branch, Environment Canada, 4905 Dufferin Street, Toronto, Ontario, Canada</addr-line>
</aff>
<pub-date pub-type="epub">
<day>27</day>
<month>08</month>
<year>2010</year>
</pub-date>
<volume>10</volume>
<issue>8</issue>
<fpage>20303</fpage>
<lpage>20327</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-discuss.net/10/20303/2010/acpd-10-20303-2010.html">This article is available from http://www.atmos-chem-phys-discuss.net/10/20303/2010/acpd-10-20303-2010.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys-discuss.net/10/20303/2010/acpd-10-20303-2010.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys-discuss.net/10/20303/2010/acpd-10-20303-2010.pdf</self-uri>
<abstract>
<p>On 30 August 2009, intense forest fires in interior BC, together with
synoptic scale meteorological subsidence and easterly winds resulted in
transport of a broad forest fire plume across southwestern BC. The
physico-chemical and optical characteristics of the plume as observed from
Saturna island (AERONET), CORALNet-UBC and the Whistler Mountain air
chemistry facility were consistent with forest fire plumes that have been
observed elsewhere in continental North America. However, the importance of
smoke plume subsidence in relation to the interpretation of mountaintop
chemistry observations is highlighted on the basis of deployment both a
&lt;i&gt;CL31&lt;/i&gt; ceilometer and a single particle mass spectrometer (SPMS) in a mountainous
setting. The SPMS was used to identify the biomass plume based on
levoglucosan and potassium markers. Data from the SPMS are also used to
show that the biomass plume was correlated with nitrate, but not correlated
with sulphate or sodium. This study not only provides baseline measurements
of biomass burning plume physico-chemical characteristics in western Canada,
but also highlights the importance of &lt;i&gt;lidar&lt;/i&gt; remote sensing methods in the
interpretation of mountaintop chemistry measurements.</p>
</abstract>
<counts><page-count count="25"/></counts>
</article-meta>
</front>
<body/>
<back>
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