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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>6</volume_number>
		<issue_number>4</issue_number>
		<publication_year>2006</publication_year>
	</journal>
	<doi>10.5194/acpd-6-7945-2006</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/6/7945/2006/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/6/7945/2006/acpd-6-7945-2006.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/6/7945/2006/acpd-6-7945-2006.pdf</fulltext_pdf>
	<start_page>7945</start_page>
	<end_page>7958</end_page>
	<publication_date>2006-08-16</publication_date>
	<article_title content_type="html">Satellite monitoring of different vegetation types by differential optical absorption spectroscopy (DOAS) in the red spectral range</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>T. Wagner</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>S. Beirle</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>M. Grzegorski</name>
		</author>
		<author numeration="4" affiliations="">
			<name>U. Platt</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Institut für Umweltphysik, University of Heidelberg, Heidelberg, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">A new method for the satellite remote sensing of different types of
vegetation and ocean colour is presented. In contrast to existing
algorithms, our method analyses weak narrow-band reflectance structures
(i.e.&amp;nbsp;&quot;fingerprint&quot; structures) of vegetation in the red spectral range. It
is based on differential optical absorption spectroscopy (DOAS), which is
usually applied for the analysis of atmospheric trace gas absorptions. Since
the spectra of atmospheric absorption and vegetation reflectance are
simultaneously included in the analysis, the effects of atmospheric
scattering and absorption are automatically corrected. The inclusion of the
vegetation spectra also significantly improves the results of the trace gas
retrieval. The global maps of the fitting coefficients for the vegetation
spectra (indicating the fraction of the observed ground scene covered by
vegetation) illustrate the seasonal cycle of different vegetation types. In
addition to the vegetation distribution on land, they also show patterns of
biological activity in the oceans. Our results indicate that improved sets
of vegetation spectra might lead to more accurate and more specific
identification of vegetation type in the future.</abstract>
	<references>
	</references>
</article>

