Intended as an overview aimed at potential users of remotely sensed sp
atial distributions and temporal variations of soil moisture, this pap
er begins with an introductory section on the fundamentals of radar im
aging and associated attributes. To place the soil moisture sensing ta
sk in proper perspective, the prerequisite step of classifying terrain
into four basic types-bare surfaces, short vegetation, tall vegetatio
n, and urban-is addressed by demonstrating how a dual-frequency polari
metric radar can correctly classify terrain with an accuracy greater t
han 90%. Over 5000 image pixels with known terrain identity were invol
ved in the evaluation of the radar image classifier. For bare soil (wi
th vegetation cover shorter than 15 cm), radar can estimate the volume
tric moisture content (expressed in per cent) of the top 5 cm soil lay
er with an r.m.s. error of 3.5%. Based on theoretical model prediction
s as well as experimental observations, strong evidence exists in supp
ort of radar's potential for sensing soil moisture under vegetation co
ver, but no operational algorithm exists at present.