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Record #122824:
Geometry and flow conditions of subglacial water at South Cascade Glacier, Washington state, U.S.A.; an analysis of tracer injections / Andrew G. Fountain.
Title: | Geometry and flow conditions of subglacial water at South Cascade Glacier, Washington state, U.S.A.; an analysis of tracer injections / Andrew G. Fountain. |
Author(s): | Fountain, Andrew G. |
Date: | 1993. |
In: | Journal of Glaciology. (1993.), Vol. 39(131) (1993) |
Abstract: | Results indicate that two distinct drainage basins on glacier feed two main streams flowing from glacier. These are described. Study differs from previous tracer studies in that results are compared to model in which velocity and dispersion result from mechanics of flow rather than as adjustable parameters. This allows estimate of path length, water depth and channel width. Flow condition of conduit can be determined from relation between travel time of tracer and water discharge. |
Notes: | Journal of Glaciology. Vol. 39(131) :143-156 (1993). |
Keywords: | 551.32 -- Glaciology. 551.324 -- Land ice. 551.324.22 -- Glaciers. 551.324.86 -- Glacier streams: South Cascade Glacier. 551.579.3 -- Water supply from glaciers. 556 -- Hydrology. E11 -- Glaciology: glaciohydrology. (73) -- United States. (79) -- Pacific states. |
SPRI record no.: | 122824 |
LDR 01533naa#a2200000#a#4500 001 SPRI-122824 005 20231130133151.0 007 ta 008 231130s1993####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-122824 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aFountain, Andrew G. 245 10 ‡aGeometry and flow conditions of subglacial water at South Cascade Glacier, Washington state, U.S.A.; an analysis of tracer injections /‡cAndrew G. Fountain. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1993. 300 ## ‡ap. 143-156 :‡bdiags., tables, maps. 500 ## ‡aJournal of Glaciology. Vol. 39(131) :143-156 (1993). 520 3# ‡aResults indicate that two distinct drainage basins on glacier feed two main streams flowing from glacier. These are described. Study differs from previous tracer studies in that results are compared to model in which velocity and dispersion result from mechanics of flow rather than as adjustable parameters. This allows estimate of path length, water depth and channel width. Flow condition of conduit can be determined from relation between travel time of tracer and water discharge. 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a551.324 -- Land ice.‡2udc 650 07 ‡a551.324.22 -- Glaciers.‡2udc 650 07 ‡a551.324.86 -- Glacier streams: South Cascade Glacier.‡2udc 650 07 ‡a551.579.3 -- Water supply from glaciers.‡2udc 650 07 ‡a556 -- Hydrology.‡2udc 650 07 ‡aE11 -- Glaciology: glaciohydrology.‡2local 651 #7 ‡a(73) -- United States.‡2udc 651 #7 ‡a(79) -- Pacific states.‡2udc 773 0# ‡7nnas ‡tJournal of Glaciology. ‡gVol. 39(131) (1993) ‡wSPRI-20534 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20231130