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Record #129756:
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Main publication details
MARC recordGlacier modeling and the climate of Patagonia during the last glacial maximum / Nick Hulton, David E. Sugden, Antony J. Payne, Chalmers M. Clapperton.
| Title: | Glacier modeling and the climate of Patagonia during the last glacial maximum / Nick Hulton, David E. Sugden, Antony J. Payne, Chalmers M. Clapperton. |
| Author(s): | Hulton, Nick. Sugden, David E. Payne, Antony J. Clapperton, Chalmers M. |
| Date: | 1994. |
| In: | Quaternary Research. (1994.), Vol. 42(1) (1994) |
| Abstract: | Describes model which is time-dependent and is driven by changing mass-balance/altitude relationship. Assuming that limits of Patagonian ice cap at last glaciation are known, it is possible to identify modelled climatic changes that are necessary to grow ice cap of extent similar to its maximum limits. Although idea of using empirical evidence to constrain theoretical models is relatively simple, it necessitates assumptions which may be difficult to validate at present. |
| Notes: | Quaternary Research. Vol. 42(1) :1-19 (1994). |
| 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. 551.583.3 -- Climatic changes, Quaternary. 551.588.5 -- Climate, relationship with ice. 519.673 -- Modelling. .000(410) -- British author. E9 -- Glaciology: meteorology and climatology. (82) -- Argentina. (83) -- Chile. (834.4) -- Aysen. (834.5) -- Magallanes. |
| SPRI record no.: | 129756 |
LDR 01787naa#a2200000#a#4500 001 SPRI-129756 005 20240418205615.0 007 ta 008 240418s1994####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-129756 040 ## ‡aUkCU-P‡beng‡eaacr 245 00 ‡aGlacier modeling and the climate of Patagonia during the last glacial maximum /‡cNick Hulton, David E. Sugden, Antony J. Payne, Chalmers M. Clapperton. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1994. 300 ## ‡ap. 1-19 :‡bdiags., map. 500 ## ‡aQuaternary Research. Vol. 42(1) :1-19 (1994). 520 3# ‡aDescribes model which is time-dependent and is driven by changing mass-balance/altitude relationship. Assuming that limits of Patagonian ice cap at last glaciation are known, it is possible to identify modelled climatic changes that are necessary to grow ice cap of extent similar to its maximum limits. Although idea of using empirical evidence to constrain theoretical models is relatively simple, it necessitates assumptions which may be difficult to validate at present. 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 ‡a551.583.3 -- Climatic changes, Quaternary.‡2udc 650 07 ‡a551.588.5 -- Climate, relationship with ice.‡2udc 650 07 ‡a519.673 -- Modelling.‡2udc 650 07 ‡a.000(410) -- British author.‡2udc 650 07 ‡aE9 -- Glaciology: meteorology and climatology.‡2local 651 #7 ‡a(82) -- Argentina.‡2udc 651 #7 ‡a(83) -- Chile.‡2udc 651 #7 ‡a(834.4) -- Aysen.‡2udc 651 #7 ‡a(834.5) -- Magallanes.‡2udc 700 1# ‡aHulton, Nick. 700 1# ‡aSugden, David E. 700 1# ‡aPayne, Antony J. 700 1# ‡aClapperton, Chalmers M. 773 0# ‡7nnas ‡tQuaternary Research. ‡gVol. 42(1) (1994) ‡wSPRI-46567 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240418