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Record #111402:

Scale dependent albedo variations and runoff from a glacierized alpine basin / Melinda M. Brugman.

Title: Scale dependent albedo variations and runoff from a glacierized alpine basin / Melinda M. Brugman.
Author(s): Brugman, Melinda M.
Date: 1991.
Publisher: Wallingford, Oxfordshire: IAHS Press
In: Snow, hydrology and forests in high alpine areas. Proceedings of an international symposium held during the 20th General Assembly of the International Union of Geodesy and Geophysics at Vienna, 11-24 August 1991. (1991.),
Abstract: Measurements made during summer 1990 on Sentinel Glacier, British Columbia. Albedo at 1 m height varied from 0.1 to 0.3 in ablation zone, 0.2 to 0.6 near equilibrium line, 0.6 to 0.8 in accumulation zone, and 0.2 to 0 in crevassed areas. Snow ablation can be explained primarily by net radiation flux, even though snowmelt and runoff peaks occur after radiation peak by several hours. Dramatic summertime albedo variations affect glacier runoff and mass balance annually, particularly below equilibrium line.
Notes:

In: Snow, hydrology and forests in high alpine areas. Proceedings of an international symposium held during the 20th General Assembly of the International Union of Geodesy and Geophysics at Vienna, 11-24 August 1991 / Heinz Bergmann, H. Lang, W. Frey, D. Issler, Bruno Salm, eds.

Keywords: 551.32 -- Glaciology.
551.324 -- Land ice.
551.324.22 -- Glaciers.
551.324.414 -- Land ice, radiation to and from.
551.578.46 -- Snow cover and snow patches.
551.521 -- Radiation, atmospheric.
551.521.32 -- Albedo. Radiation, terrestrial and atmospheric.
551.578.462 -- Snow cover, ablation.
E10 -- Glaciology: snow and avalanches.
(*41) -- Canada.
(*429) -- British Columbia.
SPRI record no.: 111402

MARCXML

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001 SPRI-111402
005 20221002040212.0
007 ta
008 221002s1991####enkab##|#####|1||#0#eng#d
035 ## ‡aSPRI-111402
040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aBrugman, Melinda M.
245 10 ‡aScale dependent albedo variations and runoff from a glacierized alpine basin /‡cMelinda M. Brugman.
260 ## ‡aWallingford, Oxfordshire :‡bIAHS Press,‡c1991.
300 ## ‡ap. 61-71 :‡bill., diags., map.
490 0# ‡aIAHS Publication ;‡v205
500 ## ‡aIn: Snow, hydrology and forests in high alpine areas. Proceedings of an international symposium held during the 20th General Assembly of the International Union of Geodesy and Geophysics at Vienna, 11-24 August 1991 / Heinz Bergmann, H. Lang, W. Frey, D. Issler, Bruno Salm, eds.
520 3# ‡aMeasurements made during summer 1990 on Sentinel Glacier, British Columbia. Albedo at 1 m height varied from 0.1 to 0.3 in ablation zone, 0.2 to 0.6 near equilibrium line, 0.6 to 0.8 in accumulation zone, and 0.2 to 0 in crevassed areas. Snow ablation can be explained primarily by net radiation flux, even though snowmelt and runoff peaks occur after radiation peak by several hours. Dramatic summertime albedo variations affect glacier runoff and mass balance annually, particularly below equilibrium line.
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.324 -- Land ice.‡2udc
650 07 ‡a551.324.22 -- Glaciers.‡2udc
650 07 ‡a551.324.414 -- Land ice, radiation to and from.‡2udc
650 07 ‡a551.578.46 -- Snow cover and snow patches.‡2udc
650 07 ‡a551.521 -- Radiation, atmospheric.‡2udc
650 07 ‡a551.521.32 -- Albedo. Radiation, terrestrial and atmospheric.‡2udc
650 07 ‡a551.578.462 -- Snow cover, ablation.‡2udc
650 07 ‡aE10 -- Glaciology: snow and avalanches.‡2local
651 #7 ‡a(*41) -- Canada.‡2udc
651 #7 ‡a(*429) -- British Columbia.‡2udc
773 0# ‡7nnam ‡aHeinz Bergmann, H. Lang, W. Frey, D. Issler, Bruno Salm, eds. ‡tSnow, hydrology and forests in high alpine areas. Proceedings of an international symposium held during the 20th General Assembly of the International Union of Geodesy and Geophysics at Vienna, 11-24 August 1991. ‡dWallingford, Oxfordshire : IAHS Press, 1991. ‡wSPRI-111397
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20221002