Improving Alpine-Region Spectral Unmixing with Optimal-Fit Snow Endmembers

Painter, T. H.; Roberts, D. A.; Green, R. O.; Dozier, J.

dc.contributor.author	Painter, T. H.	en_US
dc.contributor.author	Roberts, D. A.	en_US
dc.contributor.author	Green, R. O.	en_US
dc.contributor.author	Dozier, J.	en_US
dc.date.accessioned	2004-10-05T06:44:07Z
dc.date.available	2004-10-05T06:44:07Z
dc.date.issued	1995--January	en_US
dc.identifier.citation	Pasadena, California, USA	en_US
dc.identifier.clearanceno	94-1621	en_US
dc.identifier.uri	http://hdl.handle.net/2014/33643
dc.description.abstract	Surface albedo and snow-covered-area (SCA) are crucial inputs to the hydrologic and climatologic modeling of alpine and seasonally snow-covered areas (Dozier, 1989). Because the spectral albedo and thermal regime of pure snow depend on grain size, areal distribution of snow grain size is required.	en_US
dc.format.extent	181039 bytes
dc.format.mimetype	application/pdf
dc.language.iso	en_US
dc.subject.other	snow grain size snow-covered-area (SCA) albedo Mammoth Mountain	en_US
dc.title	Improving Alpine-Region Spectral Unmixing with Optimal-Fit Snow Endmembers	en_US