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General EB Components in EEFlux – <br />from METRIC (Mapping ET at high Resolution using <br />Inverse Calibration) <br />Net Radiation (Rn) <br />Reflected shortwave from satellite <br />Incoming shortwave from theory <br />Emitted longwave from satellite <br />Incoming longwave from emitted and atmospheric transmissivity <br />Sensible Heat Flux (H) <br />Near surface vertical air temperature gradient (dT) keyed from surface <br />temperature (Ts) – calibrated to each image date (dT = a + b Ts) <br />Aerodynamic resistance from <br />Wind speed at blending height (from gridded or local weather) <br />Aerodynamic roughness from vegetation indices and land use type <br />Buoyancy effects from iterative solutions <br />Soil Heat Flux (G) <br />Function of H for nearly bare soil and function of Rn for vegetation <br /> <br />λE = Rn – G - H