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Record #179571:

Spatial and temporal variations in the thermodynamics since the last glacial maximum at Jutulstraumen drainage basin, East Antarctica / C. Rolstad.

Title: Spatial and temporal variations in the thermodynamics since the last glacial maximum at Jutulstraumen drainage basin, East Antarctica / C. Rolstad.
Author(s): Rolstad, C.
Date: 2006.
In: Norsk Geografisk Tidsskrift. (2006.), Vol. 60 (2006)
Abstract: Uses flow-line model coupled to 2D temperature model to simulate thermodynamic changes of Jutulstraumen drainage basin due to grounding line retreat and increased surface temperature since last glacial maximum (LGM). Basin consists of plateau drained by outlet glacier, and simulated ice volume reductions are 1% and 2% respectively of current grounded volume. Present-day glacier is almost in balance with current climate, and simulated thermal regime of outlet glacier shows basal layer at pressure melting point and negative temperature gradients with depth due to horizontal advection of cold ice from plateau. Sensitivity studies show that strain heating and horizontal advection are important for basal temperatures in fast flowing outlet glacier and for about half of wide basin at polar plateau. Increased strain heating and horizontal advection since LGM control response time required to readjust to new conditions, and control present-day volume.
Notes:

Norsk Geografisk Tidsskrift. Vol. 60 :139-148 (2006).

Keywords: 551.32 -- Glaciology.
551.324 -- Land ice.
551.324.22 -- Glaciers.
551.324.41 -- Land ice, thermal balance.
551.324.43 -- Land ice, regime and mass balance.
551.324.6 -- Land ice, fluctuation.
551.324.63 -- Land ice, advance and retreat.
551.336 -- Ice ages.
551.321.8 -- Glaciological model experiments.
E5 -- Glaciology: land ice.
(*7) -- Antarctic regions.
(*73) -- Dronning Maud Land.
(*732) -- Kronprinsesse Martha Kyst.
(*733) -- Prinsesse Astrid Kyste.
SPRI record no.: 179571

MARCXML

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100 1# ‡aRolstad, C.
245 10 ‡aSpatial and temporal variations in the thermodynamics since the last glacial maximum at Jutulstraumen drainage basin, East Antarctica /‡cC. Rolstad.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2006.
300 ## ‡ap. 139-148 :‡bill., diags., maps.
500 ## ‡aNorsk Geografisk Tidsskrift. Vol. 60 :139-148 (2006).
520 3# ‡aUses flow-line model coupled to 2D temperature model to simulate thermodynamic changes of Jutulstraumen drainage basin due to grounding line retreat and increased surface temperature since last glacial maximum (LGM). Basin consists of plateau drained by outlet glacier, and simulated ice volume reductions are 1% and 2% respectively of current grounded volume. Present-day glacier is almost in balance with current climate, and simulated thermal regime of outlet glacier shows basal layer at pressure melting point and negative temperature gradients with depth due to horizontal advection of cold ice from plateau. Sensitivity studies show that strain heating and horizontal advection are important for basal temperatures in fast flowing outlet glacier and for about half of wide basin at polar plateau. Increased strain heating and horizontal advection since LGM control response time required to readjust to new conditions, and control present-day volume.
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.324 -- Land ice.‡2udc
650 07 ‡a551.324.22 -- Glaciers.‡2udc
650 07 ‡a551.324.41 -- Land ice, thermal balance.‡2udc
650 07 ‡a551.324.43 -- Land ice, regime and mass balance.‡2udc
650 07 ‡a551.324.6 -- Land ice, fluctuation.‡2udc
650 07 ‡a551.324.63 -- Land ice, advance and retreat.‡2udc
650 07 ‡a551.336 -- Ice ages.‡2udc
650 07 ‡a551.321.8 -- Glaciological model experiments.‡2udc
650 07 ‡aE5 -- Glaciology: land ice.‡2local
651 #7 ‡a(*7) -- Antarctic regions.‡2udc
651 #7 ‡a(*73) -- Dronning Maud Land.‡2udc
651 #7 ‡a(*732) -- Kronprinsesse Martha Kyst.‡2udc
651 #7 ‡a(*733) -- Prinsesse Astrid Kyste.‡2udc
773 0# ‡7nnas ‡tNorsk Geografisk Tidsskrift. ‡gVol. 60 (2006) ‡wSPRI-13025
916 ## ‡a2007/07/27 -- HS
917 ## ‡aUnenhanced record from Muscat, imported 2019
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