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<article language="en">
	<journal>
		<journal_title>Atmospheric Measurement Techniques Discussions</journal_title>
		<journal_url>www.atmos-meas-tech-discuss.net</journal_url>
		<eissn>1867-8610</eissn>
		<volume_number>3</volume_number>
		<issue_number>3</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/amtd-3-2367-2010</doi>
	<article_url>http://www.atmos-meas-tech-discuss.net/3/2367/2010/</article_url>
	<abstract_html>http://www.atmos-meas-tech-discuss.net/3/2367/2010/amtd-3-2367-2010.html</abstract_html>
	<fulltext_pdf>http://www.atmos-meas-tech-discuss.net/3/2367/2010/amtd-3-2367-2010.pdf</fulltext_pdf>
	<start_page>2367</start_page>
	<end_page>2387</end_page>
	<publication_date>2010-05-28</publication_date>
	<article_title content_type="html">Columnar aerosol size distribution function obtained by inversion of spectral optical depth measurements for the Zanjan, Iran</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>A. Masoumi</name>
			<email>masoumi@iasbs.ac.ir</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>A. Bayat</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>H. R. Khalesifard</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Institute for Advanced Studies in Basic Sciences (IASBS), P.O. Box  45195-1159, Zanjan, 45195, Iran</affiliation>
	</affiliations>
	<abstract content_type="html">We are reporting the calculated values of columnar aerosol size distribution
function for atmosphere of Zanjan, a city in Northwest Iran
(36.70° N, 48.51° E). Ground-based measurements of the total
optical depth of the Zanjan atmosphere at 440 nm, 670 nm, 870 nm, and
1020 nm are recorded using a Cimel CE318-2 sunphotometer in the period of
October 2006 to September 2008. The spectral aerosol optical depth has been
obtained by subtraction of molecular optical depth from the total optical
depth for each wavelength channel. Also the Ångström exponent is
determined by a logarithmic fit to the aerosol optical depth when it is
plotted versus the logarithm of the wavelength. Daily averages of the
measured aerosol optical depth and Ångström exponent values have been
implemented in an inversion algorithm for calculation of the columnar aerosol
size distribution function. In this algorithm, the aerosols are considered as
spheres of different size and refractive index of 1.45. We found that for
82% of the days, aerosols are in the coarse mode. For these days, more than
50% of the aerosol volume concentration has a radius &amp;gt;1 &amp;mu;m. We
believe this is related to the geographical location of Zanjan in a mostly
dry area and subject to frequent dust winds.</abstract>
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</article>

