HR: 0800h
AN: C31A-0307    [Abstracts]
TI: Snowmelt in a High Latitude Mountain Catchment: Effect of Vegetation Cover and Elevation
AU: * Pomeroy, J W
EM: pomeroy@usask.ca
AF: University of Saskatchewan, Centre for Hydrology, University of Saskatchewan, Saskatoon, SK S7N 5C8 Canada
AU: Essery, R L
EM: rie@aber.ac.uk
AF: University of Wales, Centre for Glaciology, University of Wales, Aberystwyth, SY23 3DB United Kingdom
AU: Ellis, C R
EM: cre152@mail.usask.ca
AF: University of Saskatchewan, Centre for Hydrology, University of Saskatchewan, Saskatoon, SK S7N 5C8 Canada
AU: Hedstrom, N R
EM: newell.hedstrom@ec.gc.ca
AF: National Water Research Institute, Environment Canada, 11 Innovation Blvd., Saskatoon, SK S7N 3H5 Canada
AU: Janowicz, R
EM: Richard.Janowicz@gov.yk.ca
AF: Yukon Environment, Water Resources Branch, Yukon Environment, 300 Main Street, Whitehorse, YT Y1A 2C6 Canada
AU: Granger, R J
EM: raoul.granger@ec.gc.ca
AF: National Water Research Institute, Environment Canada, 11 Innovation Blvd., Saskatoon, SK S7N 3H5 Canada
AB: The energetics and mass balance of snowpacks in the premelt and melt period were compared from three elevation bands in a high latitude mountain catchment, Wolf Creek Research Basin, Yukon. Elevation is strongly correlated with vegetation cover and in this case the three elevation bands (low, middle, high) correspond to mature spruce forest, dense shrub tundra and sparse tundra (alpine). Measurements of radiation, ground heat flux, snow depth, snowfall, air temperature, wind speed were made on a half-hourly basis at the three elevations for a 10 year period. Sondes provided vertical gradients of air temperature, humidity, wind speed and air pressure. Snow depth and density surveys were conducted monthly. Comparisons of wind speed, air temperature and humidity at three elevations show that the expected elevational gradients in the free atmosphere were slightly enhanced just above the surface canopies, but that the climate at the snow surface was further influenced by complex canopy effects. Premelt snow accumulation was strongly affected by intercepted snow in the forest and blowing snow sublimation in the sparse tundra but not by the small elevational gradients in snowfall. As a result the maximum premelt SWE was found in the mid-elevation shrub tundra and was roughly double that of the sparse tundra or forest. Minimum variability of SWE was observed in the forest and shrub tundra (CV=0.25) while in the sparse tundra variability doubled (CV=0.5). Snowmelt was influenced by differences in premelt accumulation as well as differences in the net energy fluxes to snow. Elevation had a strong effect on the initiation of melt with the forest melt starting on average 16 days before the shrub tundra and 19 days before the sparse tundra. Mean melt rates showed a maximum in middle elevations and increased from 860 kJ/day in the forest to 1460 kJ/day in the sparse tundra and 2730 kJ/day in the shrub tundra. The forest canopy reduced melt while the shrub canopy enhanced it relative to the sparsely vegetated tundra. Duration of melt was similar in the forest and shrub tundra at 20 days while the sparse tundra was shorter at 13 days; the differences due to differing snow accumulation and melt rates. The greatest variability in the timing and rate of melt was found in the shrub tundra, where the effect of the shrub canopy over snow depends on snow depth and insolation and is reduced in years with high snow accumulation or extensive cloudy periods in spring. The results show that it is necessary to consider the combination of elevation and vegetation effects on snow microclimate and melt processes in high latitude mountain catchments, but that weather patterns induce substantial variability on the effect these factors.
DE: 3322 Land/atmosphere interactions
DE: 3307 Boundary layer processes
DE: 1833 Hydroclimatology
DE: 1860 Runoff and streamflow
DE: 1878 Water/energy interactions
SC: Cryosphere [C]
MN: 2004 AGU Fall Meeting