Water Stewardship Information Sources

ID 1848
Citation Déry S.J., Clifton A., Macleod S. and Beedle M.J. (2010) Blowing snow fluxes in the caribou Mountains of British Columbia, Canada, Arctic, Antarctic and Alpine Research 42, pp. 188–197. DOI:10.1657/1938-4246-42.2.188
Organization University of Northern British Columbia; SLF Davos; Goldcorp Canada-Equite Silver
URL http://www.unbc.ca/sites/default/files/assets/quesnel_river_research_centre/blowing_copy2.pdf
Abstract/Description or Keywords The Cariboo Mountains form the northern extension of the Columbia Mountains, spanning a distance of about 300 km in central British Columbia (BC), Canada. Cool air temperatures, abundant snowfall, and strong winds (especially above treeline and along exposed ridges) would suggest frequent and intense blowing snow events. The occurrence of intense blowing snow episodes is confirmed by automated wind and snow depth measurements at several sites in the area. Simulations conducted with a numerical model forced by meteorological observations recorded from 2006 to 2009 reveal a high frequency of blowing snow episodes at three high-elevation sites in the Cariboo Mountains. This process is especially prominent on the exposed ridge of Browntop Mountain (elevation of 2031 m a.s.l.) where snow transport by wind is calculated to occur as much as two-thirds of the time during some winter months. Simulated blowing snow fluxes remain high at this site with monthly transport and sublimation rates reaching 5301 Mg m21 and 31 mm snow water equivalent (SWE), respectively. Blowing snow is also shown to be a dominant process in snow accumulation at the upper Castle Creek Glacier site (elevation of 2105 m a.s.l.), with strong winds generating sharp declines in snow depth and the erosion of more than 200 cm of snow depth during two successive winters. The results presented in this study suggest that blowing snow contributes significantly to snow accumulation and the mass balance of glaciers in BC’s Cariboo Mountains.
Information Type Article
Regional Watershed Quesnel River
Sub-watershed if known
Aquifer #
Comments
Project status
Contact Name Stephen J. Dery
Contact Email [email protected]