Two radar experiments were performed in the French Alps in December 19
89 and April 1990. The main objective was to study the signature of sn
ow-covered terrain for different snow conditions. The E-SAR (Band X) f
rom DLR was used, and the data were processed by CNES. The study area
was situated at Les Arcs, a ski resort, with elevations ranging from 1
600 m to 2600 m. Ground data included snow depth, liquid water content
, and snow and air temperature. A SPOT image was available for Decembe
r and aerial photographs for the following July. In December there was
almost no snow, while in April the area was completely snow covered.
Because of the highly varying topography, a DEM (digital elevation mod
el) was used to correct the image geometrically and radiometrically. A
simple scheme was developed for these corrections. The snow was sligh
tly wet in April and many features appearing on the image are due to t
he snow itself or to the snow-ground interface. In particular, the ski
runs are clearly visible due to the different structure of the packed
snow. Only a small area could be compared between December and April
due to technical problems in December. It appears that the snow-free a
nd snow-covered signatures are very similar for this particular terrai
n, which is a golf course in summer; that is, smooth wet soil with sho
rt grass. These experiments show that are necessary when studying moun
tainous area. Furthermore calibrated data are required to compare snow
-free and snow-covered terrain when the snow is slightly wet and there
fore slightly absorbant with respect to the electromagnetic waves.