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Record #117997:
- #117997
Main publication details
MARC recordThe western Barents Sea and the Svalbard archipelago 18 000 years ago -- a finite-difference computer model reconstruction / Elisabeth Isaksson.
| Title: | The western Barents Sea and the Svalbard archipelago 18 000 years ago -- a finite-difference computer model reconstruction / Elisabeth Isaksson. |
| Author(s): | Isaksson, Elisabeth. |
| Date: | 1992. |
| In: | Journal of Glaciology. (1992.), Vol. 38(129) (1992) |
| Abstract: | One-dimensional finite-difference model used to reconstruct steady-state ice sheet over this area at last glacial maximum. Model reconstructs ice-surface elevation as output based on information about glacial geology, bed topography, basal conditions, mass balance, flow-band width, ice-stream length, and flow-law constraints. Result suggests marine ice dome 1700 m high east of Spitsbergen and terrestrial dome 1350 m high over north-west Spitsbergen. |
| Notes: | Journal of Glaciology. Vol. 38(129) :295-301 (1992). |
| Keywords: | 551.336 -- Ice ages. 551.79 -- Quaternary. 519.673 -- Modelling. E7 -- Glaciology: glacial geology and ice ages. (*60) -- Arctic Ocean and adjacent waters. (*686) -- Barents Sea. (*3) -- Arctic regions. (*32) -- Svalbard. (*324) -- Spitsbergen. |
| SPRI record no.: | 117997 |
LDR 01457naa#a2200000#a#4500 001 SPRI-117997 005 20230926124656.0 007 ta 008 230926s1992####xx#b##|##|###|0||#0|eng#d 035 ## ‡aSPRI-117997 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aIsaksson, Elisabeth. 245 14 ‡aThe western Barents Sea and the Svalbard archipelago 18 000 years ago -- a finite-difference computer model reconstruction /‡cElisabeth Isaksson. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1992. 300 ## ‡ap. 295-301 :‡bmaps. 500 ## ‡aJournal of Glaciology. Vol. 38(129) :295-301 (1992). 520 3# ‡aOne-dimensional finite-difference model used to reconstruct steady-state ice sheet over this area at last glacial maximum. Model reconstructs ice-surface elevation as output based on information about glacial geology, bed topography, basal conditions, mass balance, flow-band width, ice-stream length, and flow-law constraints. Result suggests marine ice dome 1700 m high east of Spitsbergen and terrestrial dome 1350 m high over north-west Spitsbergen. 650 07 ‡a551.336 -- Ice ages.‡2udc 650 07 ‡a551.79 -- Quaternary.‡2udc 650 07 ‡a519.673 -- Modelling.‡2udc 650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local 651 #7 ‡a(*60) -- Arctic Ocean and adjacent waters.‡2udc 651 #7 ‡a(*686) -- Barents Sea.‡2udc 651 #7 ‡a(*3) -- Arctic regions.‡2udc 651 #7 ‡a(*32) -- Svalbard.‡2udc 651 #7 ‡a(*324) -- Spitsbergen.‡2udc 773 0# ‡7nnas ‡tJournal of Glaciology. ‡gVol. 38(129) (1992) ‡wSPRI-20534 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230926