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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>4</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/acpd-8-16219-2008</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/8/16219/2008/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/8/16219/2008/acpd-8-16219-2008.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/8/16219/2008/acpd-8-16219-2008.pdf</fulltext_pdf>
	<start_page>16219</start_page>
	<end_page>16254</end_page>
	<publication_date>2008-08-26</publication_date>
	<article_title content_type="html">Spatial heterogeneity of satellite derived land surface parameters and energy flux densities for LITFASS-area</article_title>
	<authors>
		<author numeration="1" affiliations="1,3">
			<name>A. Tittebrand</name>
			<email>antje.tittebrand@zmaw.de</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>F. H. Berger</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Institute for Hydrology and Meteorology, Dresden, Germany</affiliation>
		<affiliation numeration="2" content_type="html">Deutscher Wetterdienst, Meteorologisches Observatorium Lindenberg, Germany</affiliation>
		<affiliation numeration="3" content_type="html">now at: Institute for Oceanography, Hamburg, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">Remote sensing data provide area integrated information of surface
properties in different spatial or temporal resolutions according to
different sensor features. Landsat ETM+, Terra MODIS and NOAA-AVHRR surface
temperature and spectral reflectance were used to infer further surface
parameters and radiant- and energy flux densities for LITFASS-area, a
20&amp;times;20 km&lt;sup&gt;2&lt;/sup&gt; heterogeneous area in Eastern Germany, mainly characterized by
the land use types forest, crop, grass and water. Based on the
Penman-Monteith-approach the actual latent heat flux (&lt;i&gt;L.E&lt;/i&gt;), as key quantity of
the hydrological cycle, is determined for each sensor in the accordant
spatial resolution with an improved parametrization. However, using three
sensors, significant discrepancies between the inferred parameters can cause
flux distinctions resultant from differences of the sensor filter response
functions or atmospheric correction methods. The approximation of MODIS- and
AVHRR- derived surface parameters to the reference parameters of ETM (via
regression lines and histogram stretching, respectively), further the use of
accurate land use classifications (CORINE and a new Landsat-classification), and a consistent
parametrization for the three sensors were realized to obtain a uniform base
for investigations of the spatial variability. For the target area the
spatial heterogeneity is analysed investigating frequency distribution
functions (PDF) for surface parameters and energy fluxes. PDF is the most
promising way to describe subgrid heterogeneity due to the given data in
different spatial resolution. Aim of this study is to find typical
distribution pattern of parameters (albedo, NDVI) for the determination of &lt;i&gt;L.E&lt;/i&gt;
determined from the highly resolved ETM data within pixel on coarser scale
(MODIS, AVHRR). The analyses for 4 scenes in 2002 and 2003 showed that clear
distribution-pattern for forest for NDVI and albedo are found. Grass and crop
distributions show higher variability and differ significantly to each other
in NDVI but only marginal in albedo. Regarding NDVI-distribution functions NDVI was
found to be the key variable for &lt;i&gt;L.E&lt;/i&gt;-determination.</abstract>
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