In the 1998-1999 winter, the operational feasibility of using RADARSAT SAR
data to estimate the spatial distribution of snow water equivalent (SWE) in
a large hydroelectric complex managed by Hydro-Quebec (La Grande River wat
ershed) has been successfully demonstrated. This watershed is located in th
e subarctic climatic region in the north-west of the Quebec province. The v
egetation consists of moderately dense to open Black Spruce forests, open l
ands, burned lands and peat bogs. In the last few years, an original approa
ch well adapted for this region has been developed to estimate the SWE from
SAR data (ERS-1, RADARSAT). This approach is based on the fact that the sn
ow cover characteristics influence the underlying soil temperature which in
fluences the dielectric properties of the soil and then the recorded backsc
attering signal. Then, a linear relationship between the backscattering rat
ios of a winter image and a snow-free (fall) image, and the snowpack therma
l resistance (thermal insulation properties) has been established. Conseque
ntly, the algorithm infers the SWE from the estimated thermal resistance an
d the measured mean density of the snowpack. This algorithm has been implem
ented within a MapInfo(TM) application that has been named EQeau. It allows
mapping of the spatial distribution of the estimated SWE at the desired le
vel (pixel, square grid, sub-watershed). During the 1998-1999 winter, EQeau
has been used successfully in a pre-operational mode using calibrated Wide
beam images (W1) from RADARSAT. The algorithm has given mean estimated SWE
values similar to the SWE values derived from Hydro-Quebec snow transects
(relative difference between 1% and 13%). Also, the SWE increase measured f
rom January to March 1999 is clearly detected on the maps covering almost 7
7 000 km(2) The next steps will be the evaluation of the ScanSAR images and
the demonstration of the economical advantages of using RADARSAT data in a
hydrological forecasting system. Copyright (C) 1999 John Wiley & Sons, Ltd
.