A Distributed Surface Temperature and Energy Balance Model of a Semi-Arid Watershed
A simple model of surface and sub -surface soil temperature was developed at the watershed scale ( -100 km2) in a semi -arid rangeland environment. The model consisted of a linear combination of air temperature and net radiation and assumed: 1) topography controls the spatial distribution of net...
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Language: | en_US |
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Department of Hydrology and Water Resources, University of Arizona (Tucson, AZ)
1994
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Online Access: | http://hdl.handle.net/10150/617637 http://arizona.openrepository.com/arizona/handle/10150/617637 |