HR: 0800h
AN: C21A-1058 [Abstracts]
TI: Measuring Winter Precipitation in a Mountain Catchment
AU: * Winstral, A
EM: awinstra@nwrc.ars.usda.gov
AF: USDA Agricultural Research Service
Northwest Watershed Research Center, 800 Park Blvd
Suite 105, Boise, ID 83712-7716
United States
AU: Marks, D
EM: danny@nwrc.ars.usda.gov
AF: USDA Agricultural Research Service
Northwest Watershed Research Center, 800 Park Blvd
Suite 105, Boise, ID 83712-7716
United States
AU: Van Vactor, S
EM: svanvact@nwrc.ars.usda.gov
AF: USDA Agricultural Research Service
Northwest Watershed Research Center, 800 Park Blvd
Suite 105, Boise, ID 83712-7716
United States
AB:
Measuring winter precipitation (principally snowfall) in a mountain catchment is difficult. The magnitude of gauge under
catch is affected by variable density during deposition, wind speed and direction, and site conditions such as vegetation and
topography. Though numerous studies have been conducted to quantify gauge under catch as a function of wind in order to
develop correction factors, all used gauge catch at a reference site to represent 'true'
deposition. None used direct measurement of snow on the ground, and few involved measurement locations within a catchment to
sample a range of site conditions and wind exposures. In this study we evaluate data from 10 precipitation measurement
sites within a mountain catchment. Each site includes an Alter-shielded and an unshielded 8-inch Belfort-type precipitation
gauge, sonic snow depth, wind speed and direction, temperature, humidity, and solar radiation sensors. In addition, one site
includes a snow pillow, and a series of seven near by bi-weekly snow course measurements provide density estimates for the
precipitation measurement sites. Unshielded and shielded gauge catch are compared to wind corrected catch using the
dual-gauge and the WMO wind correction approaches. Snow depth is combined with snow density derived from the snow pillow and
the near-by snow courses to estimate true snow deposition near the measurement sites. This research will improve our
understanding of the relationships between precipitation, deposition, and gauge catch in mountainous regions.
DE: 0736 Snow (1827, 1863)
DE: 0740 Snowmelt
DE: 1840 Hydrometeorology
DE: 1895 Instruments and techniques: monitoring
DE: 3354 Precipitation (1854)
SC: Cryosphere [C]
MN: Fall Meeting 2005