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Record #108574:
- #108574
Main publication details
MARC recordDynamics of ice shelves and their sensitivity to changing mass-balance quantities: model results for Filchner-Ronne ice shelf, Antarctica / Jürgen Determann, Hans Oerter.
| Title: | Dynamics of ice shelves and their sensitivity to changing mass-balance quantities: model results for Filchner-Ronne ice shelf, Antarctica / Jürgen Determann, Hans Oerter. |
| Author(s): | Determann, Jürgen. Oerter, Hans. |
| Date: | 1990. |
| In: | Zeitschrift für Gletscherkunde und Glazialgeologie. (1990.), Vol. 26(1) (1990) |
| Abstract: | Published 1992 Previous evidence suggests basal layer up to 400 m thick. Attempts to demonstrate that this consists of marine ice which grew in water column beneath ice shelf. Application of finite-differences ice-flow model reveals contribution of bottom melting and accumulation to mass budget. Basal interactions also control steady-state thickness profile of ice shelf. |
| Notes: | Zeitschrift für Gletscherkunde und Glazialgeologie. Vol. 26(1) :57-68 (1990). |
| Keywords: | 551.32 -- Glaciology. 551.324 -- Land ice. 551.324.28 -- Ice shelves. 551.324.43 -- Land ice, regime and mass balance. 551.324.51 -- Land ice, theory of flow. 519.673 -- Modelling. E5 -- Glaciology: land ice. (*7) -- Antarctic regions. (*728) -- Filchner-Ronne ice shelves. |
| SPRI record no.: | 108574 |
LDR 01513naa#a2200000#a#4500 001 SPRI-108574 005 20240416152418.0 007 ta 008 240416s1990####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-108574 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aDetermann, Jürgen. 245 10 ‡aDynamics of ice shelves and their sensitivity to changing mass-balance quantities :‡bmodel results for Filchner-Ronne ice shelf, Antarctica /‡cJürgen Determann, Hans Oerter. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1990. 300 ## ‡ap. 57-68 :‡bdiags., maps. 500 ## ‡aZeitschrift für Gletscherkunde und Glazialgeologie. Vol. 26(1) :57-68 (1990). 520 3# ‡aPublished 1992 Previous evidence suggests basal layer up to 400 m thick. Attempts to demonstrate that this consists of marine ice which grew in water column beneath ice shelf. Application of finite-differences ice-flow model reveals contribution of bottom melting and accumulation to mass budget. Basal interactions also control steady-state thickness profile of ice shelf. 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a551.324 -- Land ice.‡2udc 650 07 ‡a551.324.28 -- Ice shelves.‡2udc 650 07 ‡a551.324.43 -- Land ice, regime and mass balance.‡2udc 650 07 ‡a551.324.51 -- Land ice, theory of flow.‡2udc 650 07 ‡a519.673 -- Modelling.‡2udc 650 07 ‡aE5 -- Glaciology: land ice.‡2local 651 #7 ‡a(*7) -- Antarctic regions.‡2udc 651 #7 ‡a(*728) -- Filchner-Ronne ice shelves.‡2udc 700 1# ‡aOerter, Hans. 773 0# ‡7nnas ‡tZeitschrift für Gletscherkunde und Glazialgeologie. ‡gVol. 26(1) (1990) ‡wSPRI-21702 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240416