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U.S. Department of Energy
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Natural gamma spectral peak method for snow measurement from aircraft

Conference ·
OSTI ID:4159817
The accuracy of airborne measurements of snow water equivalent over large areas using the $sup 40$K gamma radiation spectral peak is limited both by the accuracy of soil moisture estimates and by variation in general radon distributions between missions. The accuracy of the $sup 208$Tl spectral peak method is constrained only by soil moisture estimate accuracy and is therefore preferred over large areas. The use of an optimal linear combination of the $sup 40$K and $sup 208$Tl method water equivalent measurements significantly improves accuracy over small basins where only one or two flights are made. To complement current literature on gamma snow surveys, dynamic aspects of radon in both soil and atmosphere are reviewed. (auth)
Research Organization:
National Weather Service, Silver Spring, MD; comps.; SEE CODE- 4415000 National Academy of Sciences, Washington, D.C. (USA)
NSA Number:
NSA-33-007310
OSTI ID:
4159817
Report Number(s):
CONF-731201--
Country of Publication:
United States
Language:
English