Abstract
The brightness temperature of snow-covered terrain was monitored throughout the winter of 1984-1985. Radiometers operating at 1.0 GHz, 16.5 GHz, and 37.0 GHz (vertical and horizontal polarization) were used. The snow conditions varied from fine-grained to refrozen snow, and from dry snow to wetnesses of different levels. The effects of snow water equivalent, structure, and grain size were examined in a detailed manner. Based on these results, a semi-empirical brightness temperature model was developed.
Original language | English |
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Pages | 1231-1234 |
Number of pages | 4 |
Publication status | Published - 1 Dec 1989 |
MoE publication type | Not Eligible |
Event | Canadian Symposium on Remote Sensing - Vancouver, Canada Duration: 10 Jul 1989 → 14 Jul 1989 Conference number: 12 |
Conference
Conference | Canadian Symposium on Remote Sensing |
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Country/Territory | Canada |
City | Vancouver |
Period | 10/07/1989 → 14/07/1989 |