Snow-cover maps generated from surface data are based on direct measurement
s. However, they are prone to interpolation errors where climate stations a
re sparsely distributed. Snow cover is clearly discernible using satellite-
obtained optical data because of the high albedo of snow, yet the surface i
s often obscured by cloud cover. Satellite-obtained passive microwave data,
compared with optical data, is relatively unaffected by clouds; however, t
he snow-cover signature is significantly affected by melting snow and the m
icrowaves may be transparent to thin snow (<3 cm). Both optical and microwa
ve sensors have problems discerning snow beneath forest canopies. This pape
r describes a method that combines ground and satellite-derived optical and
passive microwave data to produce a multiple-dataset snow-cover product. C
omparisons with current snow-cover products show that the multiple-dataset
product draws together the advantages of each of its component products whi
le minimizing the potential errors. Improved estimates of the snow-covered
area are derived through the addition of two snow-cover classes ("thin or p
atchy" and "high elevation" snow cover) and from the analysis of the climat
e station data within each class. The compatibility of this method for use
with Moderate Resolution Imaging Spectroradiometer data, which will be avai
lable in 1999, and with Advanced Microwave Scanning Radiometer data, availa
ble in 2000, is also discussed. With the assimilation of these data, the re
solution of the multiple-dataset product would be improved both spatially a
nd temporally and the analysis would become completely automated. (C)Elsevi
er Science, Inc., 2000.