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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>6</issue_number>
		<publication_year>2003</publication_year>
	</journal>
	<doi>10.5194/acpd-3-5595-2003</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/3/5595/2003/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/3/5595/2003/acpd-3-5595-2003.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/3/5595/2003/acpd-3-5595-2003.pdf</fulltext_pdf>
	<start_page>5595</start_page>
	<end_page>5658</end_page>
	<publication_date>2003-11-11</publication_date>
	<article_title content_type="html">Multi Axis Differential Optical Absorption Spectroscopy (MAX-DOAS)</article_title>
	<authors>
		<author numeration="1" affiliations="1,2">
			<name>G. Hönninger</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>C. von Friedeburg</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>U. Platt</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Institut für Umweltphysik, Universität Heidelberg, Heidelberg, Germany</affiliation>
		<affiliation numeration="2" content_type="html">now at: Meteorological Service of Canada, Toronto, Canada</affiliation>
	</affiliations>
	<abstract content_type="html">Multi Axis Differential Optical Absorption Spectroscopy (MAX-DOAS) is a novel
      measurement technique that represents a significant advance on the well-established zenith
      scattered sunlight DOAS instruments which are mainly sensitive to stratospheric absorbers.
      MAX-DOAS utilizes scattered sunlight received from multiple viewing directions. The
      spatial distribution of various trace gases close to the instrument can be derived by combining
      several viewing directions. Ground based MAX-DOAS is highly sensitive to absorbers in the
      lowest few kilometres of the atmosphere and vertical profile information can be retrieved by
      combining the measurements with Radiative Transfer Model (RTM) calculations. The
      potential of the technique for a wide variety of studies of tropospheric trace species and its
      (few) limitations are discussed. A Monte Carlo RTM is applied to calculate Airmass Factors
      (AMF) for the various viewing geometries of MAX-DOAS. Airmass Factors can be used to
      quantify the light path length within the absorber layers. The airmass factor dependencies on
      the viewing direction and the influence of several parameters (trace gas profile, ground
      albedo, aerosol profile and type, solar zenith and azimuth angles) are investigated. In addition
      we give a brief description of the instrumental MAX-DOAS systems realised and deployed so
      far. The results of the RTM studies are compared to several examples of recent
      MAX-DOAS field experiments and an outlook for future possible applications is given.</abstract>
	<references>
	</references>
</article>

