In order to investigate the effect of the antenna gain on land surface para
meter retrievals with SSM/I, a Gauss-function is fitted to the 19 GHz anten
na gain functions. Soil moisture and surface temperature distributions for
the Red-Arkansas River basins are calculated from a soil-vegetation-atmosph
ere model. A passive microwave emission model is applied to derive polarize
d 19 GHz brightness temperatures. Those parameters are aggregated up to 19
GHz footprint size taking into account different spatial weighting accordin
g to the Gauss-function. These reference averages represent the full radiom
eter resolution, which is approximately three times the -3dB resolution. Th
e comparisons between the reference values and simple linear averages for s
everal spatial resolutions lead to differences varying from 2% to 17% volum
etric soil moisture.