The capability of mapping wet snowcovers by means of Synthetic Aperture Rad
ar (SAR) is well known. However, using only the backscattering intensity at
C-band, there still remain some incertitudes regarding the effect of eithe
r rough snow surfaces or very small liquid water contents for measurements
performed at small incidence angles. Since the European remote sensing (ERS
) satellites usually operate at 23 degrees incidence angle, it is important
to consider these effects. This paper shows that these difficulties can be
overcome using repeat-pass SAR interferometry. ERS data over a part of the
Netherlands and a part of Switzerland are used as illustrative examples. I
n the situations examined the occurrence of wet snow could not be directly
observed by means of the backscattering intensity, but the use of the degre
e of coherence allowed an easy discrimination. The results are validated wi
th in situ measurements.