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<!DOCTYPE article SYSTEM "http://www.atmos-chem-phys-discuss.net/inc/acpd/copernicus.dtd">
<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>3</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2003</publication_year>
	</journal>
	<doi>10.5194/acpd-3-615-2003</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/3/615/2003/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/3/615/2003/acpd-3-615-2003.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/3/615/2003/acpd-3-615-2003.pdf</fulltext_pdf>
	<start_page>615</start_page>
	<end_page>653</end_page>
	<publication_date>2003-02-10</publication_date>
	<article_title content_type="html">Haze in the Klang Valley of Malaysia</article_title>
	<authors>
		<author numeration="1" affiliations="1,4">
			<name>M. D. Keywood</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>G. P. Ayers</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>J. L. Gras</name>
		</author>
		<author numeration="4" affiliations="2">
			<name>R. Boers</name>
		</author>
		<author numeration="5" affiliations="3">
			<name>C. P. Leong</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">CSIRO Atmospheric Research, Australia</affiliation>
		<affiliation numeration="2" content_type="html">Atmospheric Research Division, KNMI, The Netherlands</affiliation>
		<affiliation numeration="3" content_type="html">Malaysian Meteorological Service, Malaysia</affiliation>
		<affiliation numeration="4" content_type="html">now at: California Institute of Technology, USA</affiliation>
	</affiliations>
	<abstract content_type="html">Continuous measurements of dry aerosol light scattering (Bsp) were made at two sites in the
      Klang Valley of Malaysia between December 1998 and December 2000.  In addition 24-h
      PM2.5 samples were collected on a one-day-in-six cycle and the chemical composition of the
      aerosol was determined.  Periods of excessive haze were defined as 24-h average Bsp
      values greater than 150 Mm&lt;sup&gt;-1&lt;/sup&gt; and these occurred on a number of occasions, between May and
      September 1999, during May 2000, and between July and September 2000.   The evidence for
      smoke being a significant contributor to aerosol during periods of excessive haze is discussed
      and includes features of the aerosol chemistry, the diurnal cycle of Bsp, and the coincidence
      of forest fires on Sumatra during the southwest (SW) monsoon period, as well as transport
      modelling for one week of the southwest Monsoon of 2000.  The study highlights that whilst
      transboundary smoke is a major contributor to poor visibility in the Klang Valley, smoke
      from fires on Peninsular Malaysia is also a contributor, and at all times, the domestic source
      of secondary particle production is present.</abstract>
	<references>
	</references>
</article>

