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Record #110861:

Das Fliessen von Schelfeisen - numerische Simulationen mit der Methode der finiten Differenzen / Jürgen Determann.

Title: Das Fliessen von Schelfeisen - numerische Simulationen mit der Methode der finiten Differenzen / Jürgen Determann.
Translated title: The flow of ice shelves - numerical simulations using the finite-difference method.
Author(s): Determann, Jürgen.
Date: 1991.
Language: German.
In: Berichte zur Polarforschung = Reports on Polar Research. (1991.), Vol. 83 (1991)
Abstract: Develops set of differential equations describing ice-shelf flow. Retarding mechanism allows simulation of basal friction. Reproduction of observed flow of Filchner-Ronne ice shelves allows simulation of dynamics; this inplies solving mass-conservation equation, involving accumulation and ablation rates from surface and base of ice shelf. Flow of Ekströmisen is simulated, but forecasts cannot be made because mass balance is so far unknown.
Notes:

Berichte zur Polarforschung = Reports on Polar Research. Vol. 83 :1-82 (1991).

English summary, p. 4-5.

Keywords: 551.32 -- Glaciology.
551.324 -- Land ice.
551.324.28 -- Ice shelves.
551.324.51 -- Land ice, theory of flow.
551.324.54 -- Land ice, flow of particular glaciers.
E5 -- Glaciology: land ice.
(*7) -- Antarctic regions.
(*732) -- Kronprinsesse Martha Kyst.
(*728) -- Filchner-Ronne ice shelves.
SPRI record no.: 110861

MARCXML

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040 ## ‡aUkCU-P‡beng‡eaacr
041 0# ‡ager
100 1# ‡aDetermann, Jürgen.
242 14 ‡aThe flow of ice shelves - numerical simulations using the finite-difference method.‡yeng
245 14 ‡aDas Fliessen von Schelfeisen - numerische Simulationen mit der Methode der finiten Differenzen /‡cJürgen Determann.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1991.
300 ## ‡ap. 1-82 :‡bdiags., tables, maps.
500 ## ‡aBerichte zur Polarforschung = Reports on Polar Research. Vol. 83 :1-82 (1991).
500 ## ‡aEnglish summary, p. 4-5.
520 3# ‡aDevelops set of differential equations describing ice-shelf flow. Retarding mechanism allows simulation of basal friction. Reproduction of observed flow of Filchner-Ronne ice shelves allows simulation of dynamics; this inplies solving mass-conservation equation, involving accumulation and ablation rates from surface and base of ice shelf. Flow of Ekströmisen is simulated, but forecasts cannot be made because mass balance is so far unknown.
546 ## ‡aIn German.
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.324 -- Land ice.‡2udc
650 07 ‡a551.324.28 -- Ice shelves.‡2udc
650 07 ‡a551.324.51 -- Land ice, theory of flow.‡2udc
650 07 ‡a551.324.54 -- Land ice, flow of particular glaciers.‡2udc
650 07 ‡aE5 -- Glaciology: land ice.‡2local
651 #7 ‡a(*7) -- Antarctic regions.‡2udc
651 #7 ‡a(*732) -- Kronprinsesse Martha Kyst.‡2udc
651 #7 ‡a(*728) -- Filchner-Ronne ice shelves.‡2udc
773 0# ‡7nnas ‡tBerichte zur Polarforschung = Reports on Polar Research. ‡gVol. 83 (1991) ‡wSPRI-64232
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20230330