Rl. Armstrong et Mj. Brodzik, Recent Northern Hemisphere snow extent: A comparison of data derived from visible and microwave satellite sensors, GEOPHYS R L, 28(19), 2001, pp. 3673-3676
During the past four decades much important information on Northern Hemisph
ere snow extent has been provided by the NOAA weekly snow extent charts der
ived from visible-band satellite imagery. Passive microwave satellite remot
e sensing can enhance snow measurements based on visible data alone because
of the ability to penetrate clouds, provide data during darkness and the p
otential to provide an index of snow depth or water equivalent. We compare
the fluctuation of Northern Hemisphere snow cover over the past twenty year
s using these two satellite remote sensing techniques. Results show compara
ble inter-annual variability with similar long-term hemispheric-scale trend
s indicating decreases in snow extent of approximately 0.2 percent per year
. The passive microwave snow algorithm applied in this study indicates less
snow-covered area than the visible data during fall and early winter when
the snow is shallow. New algorithms designed to reduce this apparent error
are being developed and tested.