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Record #111163:
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Main publication details
MARC recordSteady-state characteristics of the Greenland ice sheet under different climates / Anne Letréguilly, Philippe Huybrechts, Niels Reeh.
| Title: | Steady-state characteristics of the Greenland ice sheet under different climates / Anne Letréguilly, Philippe Huybrechts, Niels Reeh. |
| Author(s): | Letréguilly, Anne. Huybrechts, Philippe. Reeh, Niels. |
| Date: | 1991. |
| In: | Journal of Glaciology. (1991.), Vol. 37(125) (1991) |
| Abstract: | Ice sheet is modelled to simulate extent and volume in warmer climates and to find if it would re-form on ice-free bedrock under present climatic conditions. Uses 3-D thermo-mechanical model with fine-resolution grid. Experiments show that ice sheet is relatively stable; temperature rise of 6° is required for it to disappear completely, which means that it probably survived last interglacial. Appears that it will re-form on bare bedrock under present, or even slightly warmer, climatic conditions. |
| Notes: | Journal of Glaciology. Vol. 37(125) :149-157 (1991). |
| Keywords: | 551.32 -- Glaciology. 551.324 -- Land ice. 551.324.24 -- Ice sheets and caps. 551.324.63 -- Land ice, advance and retreat. 551.58 -- Climatology. 551.583 -- Climatic changes. 551.588.5 -- Climate, relationship with ice. E5 -- Glaciology: land ice. (*38) -- Greenland. |
| SPRI record no.: | 111163 |
LDR 01584naa#a2200000#a#4500 001 SPRI-111163 005 20231001220520.0 007 ta 008 231001s1991####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-111163 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aLetréguilly, Anne. 245 10 ‡aSteady-state characteristics of the Greenland ice sheet under different climates /‡cAnne Letréguilly, Philippe Huybrechts, Niels Reeh. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1991. 300 ## ‡ap. 149-157 :‡bdiags., tables, maps. 500 ## ‡aJournal of Glaciology. Vol. 37(125) :149-157 (1991). 520 3# ‡aIce sheet is modelled to simulate extent and volume in warmer climates and to find if it would re-form on ice-free bedrock under present climatic conditions. Uses 3-D thermo-mechanical model with fine-resolution grid. Experiments show that ice sheet is relatively stable; temperature rise of 6° is required for it to disappear completely, which means that it probably survived last interglacial. Appears that it will re-form on bare bedrock under present, or even slightly warmer, climatic conditions. 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a551.324 -- Land ice.‡2udc 650 07 ‡a551.324.24 -- Ice sheets and caps.‡2udc 650 07 ‡a551.324.63 -- Land ice, advance and retreat.‡2udc 650 07 ‡a551.58 -- Climatology.‡2udc 650 07 ‡a551.583 -- Climatic changes.‡2udc 650 07 ‡a551.588.5 -- Climate, relationship with ice.‡2udc 650 07 ‡aE5 -- Glaciology: land ice.‡2local 651 #7 ‡a(*38) -- Greenland.‡2udc 700 1# ‡aHuybrechts, Philippe. 700 1# ‡aReeh, Niels. 773 0# ‡7nnas ‡tJournal of Glaciology. ‡gVol. 37(125) (1991) ‡wSPRI-20534 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20231001