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<article language="en">
	<journal>
		<journal_title>Atmospheric Measurement Techniques</journal_title>
		<journal_url>www.atmos-meas-tech.net</journal_url>
		<issn>1867-1381</issn>
		<eissn>1867-8548</eissn>
		<volume_number>2</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/amt-2-327-2009</doi>
	<article_url>http://www.atmos-meas-tech.net/2/327/2009/</article_url>
	<abstract_html>http://www.atmos-meas-tech.net/2/327/2009/amt-2-327-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-meas-tech.net/2/327/2009/amt-2-327-2009.pdf</fulltext_pdf>
	<start_page>327</start_page>
	<end_page>335</end_page>
	<publication_date>2009-07-13</publication_date>
	<article_title content_type="html">Determination of particulate matter vertical columns using satellite observations</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>A. A. Kokhanovsky</name>
			<email>alexk@iup.physik.uni-bremen.de</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>A. S. Prikhach</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>I. L. Katsev</name>
		</author>
		<author numeration="4" affiliations="2">
			<name>E. P. Zege</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Institute of Environmental Physics, O. Hahn Allee 1, 28334 Bremen, Germany</affiliation>
		<affiliation numeration="2" content_type="html">Institute of Physics, National Academy of Sciences of Belarus, Nezavisimosti Prospekt 68, 220068, Minsk, Belarus</affiliation>
	</affiliations>
	<abstract content_type="html">A new technique to retrieve the particulate matter vertical columns from
spaceborne observations is described. The method is based on the
measurements of the spectral aerosol optical thickness (AOT). The spectral
slope of the derived aerosol optical thickness is used to infer the size of
particles, which is needed (along with the absolute value of AOT) to
determine corresponding vertical columns. The technique is applied to the
case of a cloudless atmosphere over Germany and results are compared with
ground-based observations. Several assumptions are made in the retrieval
process such as the prescribed phase function, single scattering albedo, the
refractive index of aerosol, and the half-width of the size distribution.</abstract>
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</article>

