Existing algorithms for retrieving snow water equivalent (SWE) from the Spe
cial Sensor Microwave/Imager (SSM/I) passive microwave brightness temperatu
re data were assessed and new algorithms that include physiographic and atm
ospheric data were developed for the Red River basin of North Dakota and Mi
nnesota. The frequencies of SSM/I data used are 19 GHz and 37 GHz in both h
orizontal and vertical polarization. Encouraging calibration results are ob
tained for the algorithms using multivariate regression technique and dry s
now cases of the 1989 and 1988 SSM/I data (from DMSP-F8). Similarly, valida
tion results for data not used in calibration [e.g., 1988 (1989 as calibrat
ion data), 1989 (1988 as calibration data), and 1997 (from DMSP-F10 and F13
)] are also encouraging. The nonparametric, Projection Pursuit Regression (
PPR) technique also gave good results in both stages. However, for the vali
dation stage, adding a shift parameter to all retrieval algorithms was alwa
ys necessary, possibly because of different scatter-induced darkening (caus
ed by scattering albedo), which could arise even for snowpacks of the same
thickness because snowpacks undergo different metamorphism in different win
ter years. Screening criteria are also proposed to eliminate SSM/I footprin
ts affected by large water bodies and depth-hoar-another key step toward re
liable SWE estimation from passive microwave data. (C) 2000 Elsevier Scienc
e Inc.