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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>2</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/acpd-8-6845-2008</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/8/6845/2008/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/8/6845/2008/acpd-8-6845-2008.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/8/6845/2008/acpd-8-6845-2008.pdf</fulltext_pdf>
	<start_page>6845</start_page>
	<end_page>6901</end_page>
	<publication_date>2008-04-09</publication_date>
	<article_title content_type="html">Aerosol optical properties in a rural environment near the mega-city Guangzhou, China: implications for regional air pollution and radiative forcing</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>R. M. Garland</name>
			<email>garland@mpch-Mainz.mpg.de</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>H. Yang</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>O. Schmid</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>D. Rose</name>
		</author>
		<author numeration="5" affiliations="4">
			<name>A. Nowak</name>
		</author>
		<author numeration="6" affiliations="4">
			<name>P. Achtert</name>
		</author>
		<author numeration="7" affiliations="4">
			<name>A. Wiedensohler</name>
		</author>
		<author numeration="8" affiliations="5">
			<name>N. Takegawa</name>
		</author>
		<author numeration="9" affiliations="5">
			<name>K. Kita</name>
		</author>
		<author numeration="10" affiliations="5">
			<name>Y. Miyazaki</name>
		</author>
		<author numeration="11" affiliations="5">
			<name>Y. Kondo</name>
		</author>
		<author numeration="12" affiliations="3">
			<name>M. Hu</name>
		</author>
		<author numeration="13" affiliations="3">
			<name>M. Shao</name>
		</author>
		<author numeration="14" affiliations="3">
			<name>L. Zeng</name>
		</author>
		<author numeration="15" affiliations="3">
			<name>Y. Zhang</name>
		</author>
		<author numeration="16" affiliations="1">
			<name>M. O. Andreae</name>
		</author>
		<author numeration="17" affiliations="1">
			<name>U. Pöschl</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Biogeochemistry Department, Max Planck Institute for Chemistry, Mainz, Germany</affiliation>
		<affiliation numeration="2" content_type="html">Helmholtz Center Munich, German Research Center for Environmental Health, Institute for Inhalation Biology, Neuherberg/Munich, Germany</affiliation>
		<affiliation numeration="3" content_type="html">College of Environmental Sciences, Peking University, Beijing, China</affiliation>
		<affiliation numeration="4" content_type="html">Leibniz Institute for Tropospheric Research, Leipzig, Germany</affiliation>
		<affiliation numeration="5" content_type="html">RCAST, University of Tokyo, Tokyo, Japan</affiliation>
	</affiliations>
	<abstract content_type="html">The scattering and absorption of solar radiation by atmospheric aerosols is
a key element of the Earth&apos;s radiative energy balance and climate. The
optical properties of aerosol particles are, however, highly variable and
not well characterized, especially near newly emerging mega-cities. In this
study, aerosol optical properties were measured at a regional background
site approximately 60 km northwest of the mega-city Guangzhou in southeast
China. The measurements were part of the &quot;Program of Regional Integrated
Experiments of Air Quality over the Pearl River Delta&quot; intensive campaign
(PRIDE-PRD2006), covering the period of 1&amp;ndash;30 July 2006. Scattering and
absorption coefficients of dry aerosol particles with diameters up to 10 &amp;mu;m (PM&lt;sub&gt;10&lt;/sub&gt;) were determined with a three-wavelength integrating
nephelometer and with a photoacoustic spectrometer, respectively.
&lt;br&gt;&lt;br&gt;
Averaged over the measurement campaign (arithmetic mean &amp;plusmn;standard
deviation), the total scattering coefficients were 200&amp;plusmn;133 Mm&lt;sup&gt;&amp;minus;1&lt;/sup&gt;
(450 nm), 151&amp;plusmn;103 Mm&lt;sup&gt;&amp;minus;1&lt;/sup&gt; (550 nm) and 104&amp;plusmn;72 Mm&lt;sup&gt;&amp;minus;1&lt;/sup&gt;
(700 nm) and the absorption coefficient was 34.3&amp;plusmn;26.5 Mm&lt;sup&gt;&amp;minus;1&lt;/sup&gt; (532 nm).
The average Ångström exponent was 1.46&amp;plusmn;0.21 (450 nm/700 nm)
and the average single scattering albedo was 0.82&amp;plusmn;0.07 (532 nm) with
minimum values as low as 0.5. The low single scattering albedo values
indicate a high abundance of, as well as strong sources of light absorbing
carbon (LAC). The ratio of LAC to CO concentration was highly variable
throughout the campaign, indicating a complex mix of different combustion
sources. The scattering and absorption coefficients, as well as the
Ångström exponent and single scattering albedo, exhibited pronounced
diurnal cycles, which can be attributed to boundary layer mixing effects and
enhanced nighttime emissions of LAC (diesel soot from regulated truck
traffic). The daytime average single scattering albedo of 0.87 appears to be
more suitable for climate modeling purposes than the 24-h average of 0.82,
as the latter value is strongly influenced by fresh emissions into a shallow
nocturnal boundary layer. In spite of high photochemical activity during
daytime, we found no evidence for strong local production of secondary
aerosol mass.
&lt;br&gt;&lt;br&gt;
The relatively low average mass scattering efficiency with respect to PM&lt;sub&gt;10&lt;/sub&gt;
(2.84&amp;plusmn;0.037 m&lt;sup&gt;2&lt;/sup&gt; g&lt;sup&gt;&amp;minus;1&lt;/sup&gt;, &amp;lambda;=550 nm) indicates a high
proportion of mass in the coarse particle fraction (diameter &amp;gt;1 &amp;mu;m).
During high pollution episodes, however, the Ångström exponent
exhibited a dependence on wavelength, which indicates an enhancement of the
fine particle fraction during these periods. A negative correlation between
single scattering albedo and backscatter fraction was observed and found to
affect the impact that these parameters have on aerosol radiative forcing
efficiency.</abstract>
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</article>

