Relative efficiency of land surface energy balance components
[1] The partitioning of available energy into dissipative fluxes over land surfaces is dependent on the state variable of the surface energy balance (land surface temperature) and the state variable of the surface water balance (soil moisture). The direct measurement of the turbulent fluxes is achie...
| Main Authors: | , |
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| Other Authors: | |
| Format: | Article |
| Language: | en_US |
| Published: |
American Geophysical Union (AGU)
2013
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| Online Access: | http://hdl.handle.net/1721.1/77890 https://orcid.org/0000-0002-8362-4761 |