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Record #199695:

Blowing snow fluxes in the Cariboo Mountains of British Columbia, Canada / Stephen J. Déry, and 3 others.

Title: Blowing snow fluxes in the Cariboo Mountains of British Columbia, Canada / Stephen J. Déry, and 3 others.
Author(s): Déry, Stephen J.
Date: 2010.
In: Arctic, Antarctic, and Alpine Research. (2010.), Vol. 42(2) (2010)
Abstract: Cool air temperatures, abundant snowfall, and strong winds in Cariboo Mountains of British Columbia result in intense blowing snow events, as confirmed by meteorological measurements at various sites, including atmospheric pressure, air and soil temperature, relative humidity, wind and speed direction, liquid precipitation, and snow depth, between 2006 and 2009. Results suggest that blowing snow contributes significantly to snow accumulation and mass balance of glaciers in Cariboo Mountains.
Notes:

Arctic, Antarctic, and Alpine Research. Vol. 42(2) :188-197 (2010).

Keywords: 551.32 -- Glaciology.
551.5 -- Meteorology.
551.51 -- Atmosphere. Structure, mechanics and thermodynamics.
551.578.4 -- Ice needles, sleet, falling snow and graupel.
551.578.46 -- Snow cover and snow patches.
519.673 -- Modelling.
551.556 -- Wind, effects of.
E10 -- Glaciology: snow and avalanches.
(*41) -- Canada.
(*429) -- British Columbia.
SPRI record no.: 199695

MARCXML

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040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aDéry, Stephen J.
245 10 ‡aBlowing snow fluxes in the Cariboo Mountains of British Columbia, Canada /‡cStephen J. Déry, and 3 others.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2010.
300 ## ‡ap. 188-197 :‡bill., diags., tables, maps.
500 ## ‡aArctic, Antarctic, and Alpine Research. Vol. 42(2) :188-197 (2010).
520 3# ‡aCool air temperatures, abundant snowfall, and strong winds in Cariboo Mountains of British Columbia result in intense blowing snow events, as confirmed by meteorological measurements at various sites, including atmospheric pressure, air and soil temperature, relative humidity, wind and speed direction, liquid precipitation, and snow depth, between 2006 and 2009. Results suggest that blowing snow contributes significantly to snow accumulation and mass balance of glaciers in Cariboo Mountains.
530 ## ‡aAlso issued online ‡uurn:doi:10.1657/1938-4246-42.2.188‡uhttps://dx.doi.org/10.1657/1938-4246-42.2.188
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.5 -- Meteorology.‡2udc
650 07 ‡a551.51 -- Atmosphere. Structure, mechanics and thermodynamics.‡2udc
650 07 ‡a551.578.4 -- Ice needles, sleet, falling snow and graupel.‡2udc
650 07 ‡a551.578.46 -- Snow cover and snow patches.‡2udc
650 07 ‡a519.673 -- Modelling.‡2udc
650 07 ‡a551.556 -- Wind, effects of.‡2udc
650 07 ‡aE10 -- Glaciology: snow and avalanches.‡2local
651 #7 ‡a(*41) -- Canada.‡2udc
651 #7 ‡a(*429) -- British Columbia.‡2udc
773 0# ‡7nnas ‡tArctic, Antarctic, and Alpine Research. ‡gVol. 42(2) (2010) ‡wSPRI-211524
916 ## ‡a2012/07/10 -- JHR
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20220926 ‡bJHR