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 radia...
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| Language: | en |
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The University of Arizona.
1994
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| Online Access: | http://hdl.handle.net/10150/186800 |