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<article language="en">
	<journal>
		<journal_title>Atmospheric Chemistry and Physics Discussions</journal_title>
		<journal_url>www.atmos-chem-phys-discuss.net</journal_url>
		<issn>1680-7367</issn>
		<eissn>1680-7375</eissn>
		<volume_number>8</volume_number>
		<issue_number>3</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/acpd-8-10275-2008</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/8/10275/2008/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/8/10275/2008/acpd-8-10275-2008.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/8/10275/2008/acpd-8-10275-2008.pdf</fulltext_pdf>
	<start_page>10275</start_page>
	<end_page>10300</end_page>
	<publication_date>2008-06-02</publication_date>
	<article_title content_type="html">Trans-Pacific dust events observed at Whistler, British Columbia during INTEX-B</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>I. G. McKendry</name>
			<email>ian@geog.ubc.ca</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>A M. Macdonald</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>W. R. Leaitch</name>
		</author>
		<author numeration="4" affiliations="3,5">
			<name>A. van Donkelaar</name>
		</author>
		<author numeration="5" affiliations="4">
			<name>Q. Zhang</name>
		</author>
		<author numeration="6" affiliations="3,5">
			<name>T. Duck</name>
		</author>
		<author numeration="7" affiliations="3,5">
			<name>R. V. Martin</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Dept. of Geography, The University of British Columbia, Vancouver, B.C., V6T 1Z2, Canada</affiliation>
		<affiliation numeration="2" content_type="html">Science and Technology Branch, Environment Canada, Toronto, Ontario, M3H 5T4, Canada</affiliation>
		<affiliation numeration="3" content_type="html">Dept. of Physics and Atmospheric Science, Dalhousie Univ., Halifax, NS M3J 1P3 Canada</affiliation>
		<affiliation numeration="4" content_type="html">State University of New York at Albany, Albany, NY, USA</affiliation>
		<affiliation numeration="5" content_type="html">also at: Harvard-Smithsonian Center for Astrophysics, Cambridge, MA, USA</affiliation>
	</affiliations>
	<abstract content_type="html">The meteorology and physico-chemical characteristics of aerosol associated
with two new cases of long range dust transport affecting western Canada
during spring 2006 are described. Each event showed enhancements of both
sulfate aerosol and crustal material of Asian origin. However, the events
were of quite different character and demonstrate the highly variable nature
of such events. The April event was a significant dust event with moderate
sulfate enhancement while the May event was a weak dust event with very
significant sulfate enhancement. The latter event was interesting in the
sense that it was of short duration and was quickly followed by significant
enhancement of organic material likely of regional origin. Comparison of
these two events with other documented cases extending back to 1993,
suggests that all dust events show coincident enhancements of sulfate and
crustal aerosol. However, events vary across a wide continuum based on the
magnitude of aerosol enhancements and their sulfate to calcium ratios. At
one extreme, events are dominated by highly significant crustal enhancements
(e.g. the well-documented 1998 and 2001 &quot;dust&quot; events) while at the other
are events with some dust transport, but where sulfate enhancements are of
very high magnitude (e.g. the 1993 event at Crater Lake and the 15 May 2006
event at Whistler). Other events represent a &quot;mix&quot;. It is likely that this
variability is a function of the comparative strengths of the dust and
anthropogenic SO&lt;sub&gt;2&lt;/sub&gt; sources, the transport pathway and in particular the
extent to which dust is transported across industrial SO&lt;sub&gt;2&lt;/sub&gt; sources, and
finally, meteorological and chemical processes.</abstract>
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</article>

