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

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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


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