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	<journal>
		<journal_title>Hydrology and Earth System Sciences Discussions</journal_title>
		<journal_url>www.hydrol-earth-syst-sci-discuss.net</journal_url>
		<issn>1812-2108</issn>
		<eissn>1812-2116</eissn>
		<volume_number>5</volume_number>
		<issue_number>4</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/hessd-5-1705-2008</doi>
	<article_url>http://www.hydrol-earth-syst-sci-discuss.net/5/1705/2008/</article_url>
	<abstract_html>http://www.hydrol-earth-syst-sci-discuss.net/5/1705/2008/hessd-5-1705-2008.html</abstract_html>
	<fulltext_pdf>http://www.hydrol-earth-syst-sci-discuss.net/5/1705/2008/hessd-5-1705-2008.pdf</fulltext_pdf>
	<start_page>1705</start_page>
	<end_page>1730</end_page>
	<publication_date>2008-07-01</publication_date>
	<article_title content_type="html">Estimating surface fluxes over the north Tibetan Plateau area with  ASTER imagery</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>W. Ma</name>
			<email>wqma@lzb.ac.cn</email>
		</author>
		<author numeration="2" affiliations="1,2,3">
			<name>Y. Ma</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>M. Li</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>Z. Hu</name>
		</author>
		<author numeration="5" affiliations="2">
			<name>L. Zhong</name>
		</author>
		<author numeration="6" affiliations="5">
			<name>Z. Su</name>
		</author>
		<author numeration="7" affiliations="4">
			<name>H. Ishikawa</name>
		</author>
		<author numeration="8" affiliations="1">
			<name>J. Wang</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Laboratory for Climate Environment and Disasters of Western China, Cold  and Arid Regions Environmental and Engineering Research Institute, Chinese  Academy of Sciences, Lanzhouï¿½ï¿½Gansu 730000, China</affiliation>
		<affiliation numeration="2" content_type="html">Institute of Tibetan Plateau Research, Chinese Academy of Sciences,  Beijing, China</affiliation>
		<affiliation numeration="3" content_type="html">School of Geography and Remote Sensing, Beijing Normal University, Beijing,  China</affiliation>
		<affiliation numeration="4" content_type="html">Disaster Prevention Research Institute, Kyoto University, Kyoto, Japan</affiliation>
		<affiliation numeration="5" content_type="html">International Institute for Geo-Information Science and Earth  Observation,\newline  Enschede, The Netherlands</affiliation>
	</affiliations>
	<abstract content_type="html">Surface fluxes are important boundary conditions for climatological modeling
and Asian monsoon system. The recent availability of high-resolution,
multi-band imagery from the ASTER (Advanced Space-borne Thermal Emission and
Reflection radiometer) sensor has enabled us to estimate surface fluxes.
ASTER covers a wide spectral region with 14 bands from the visible to the
thermal infrared with high spatial, spectral and radiometric resolution. The
spatial resolution varies with wavelength: 15 m in the visible and
near-infrared (VNIR), 30 m in the short wave infrared (SWIR), and 90 m in
the thermal infrared (TIR). A parameterization method based on ASTER data
and field observations has been proposed and tested for deriving surface
albedo, surface temperature, Normalized Difference Vegetation Index
(NDVI), Modified Soil Adjusted Vegetation Index (MSAVI), vegetation coverage, Leaf
Area Index (LAI), net radiation flux, soil heat flux, sensible heat flux and
latent heat flux over heterogeneous land surface in this paper. As a case
study, the methodology was applied to the experimental area of the
Coordinated Enhanced Observing Period (CEOP) Asia-Australia Monsoon Project
(CAMP) on the Tibetan Plateau (CAMP/Tibet), which located at the north
Tibetan Plateau. The ASTER data of 24 July 2001, 29 November 2001 and 12 March 2002 was used in this paper for the case of summer, winter and spring.
To validate the proposed methodology, the ground-measured surface variables
(surface albedo and surface temperature) and land surface heat fluxes (net
radiation flux, soil heat flux, sensible heat flux and latent heat flux)
were compared to the ASTER derived values. The results show that the derived
surface variables and land surface heat fluxes in three different months
over the study area are in good accordance with the land surface status.
Also, the estimated land surface variables and land surface heat fluxes are
in good accordance with ground measurements, and all their absolute percent
difference (APD) is less than 10% in the validation sites. It is
therefore concluded that the proposed methodology is successful for the
retrieval of land surface variables and land surface heat fluxes using the
ASTER data and filed observation over the study area.</abstract>
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