Determination of XE Directly from the Remote Sensing Data

Many approaches for determination of XE directly from remote-sensing data use the surface energy balance equation as the primary boundary condition to be satisfied; that is,

where Rn + G is often termed the available energy and H + XE are the turbulent fluxes. Evaluation of the available energy is relatively straightforward and will be addressed first, followed by the discussion of more complex evaluation of the turbulent fluxes H and XE.

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