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Record #150573:
High-resolution modeling of the advance of the Younger Dryas ice sheet and its climate in Scotland / Alun Hubbard.
Title: | High-resolution modeling of the advance of the Younger Dryas ice sheet and its climate in Scotland / Alun Hubbard. |
Author(s): | Hubbard, Alun. |
Date: | 1999. |
In: | Quaternary Research. (1999.), Vol. 52(1) (1999) |
Abstract: | Develops a quasi-three-dimensional, time-dependent ice flow/mass balance model for Scotland, applied at 1 km resolution. Includes essential longitudinal correction term. Reconstruction of past climatic and environmental conditions shows Scotland susceptible to glaciation after temperature depression of 2.5°C under present-day precipitation. Support is found for GRIP-style (Greenland Ice Core Project) temperature curve affecting Scotland during Younger Dryas though continued expansion under these climatic conditions conflicts with empirical evidence. |
Notes: | Quaternary Research. Vol. 52(1) :27-43 (1999). |
Keywords: | 551.32 -- Glaciology. 551.324 -- Land ice. 551.324.4 -- Land ice, mass and energy balance. 551.324.43 -- Land ice, regime and mass balance. 551.324.63 -- Land ice, advance and retreat. 551.58 -- Climatology. 551.583 -- Climatic changes. 551.579 -- Hydrometeorology. 519.673 -- Modelling. E7 -- Glaciology: glacial geology and ice ages. (411) -- Scotland. |
SPRI record no.: | 150573 |
LDR 01664naa#a2200000#a#4500 001 SPRI-150573 005 20230925150325.0 007 ta 008 230925s1999####xx#a##|##|###|0||#0|eng#d 035 ## ‡aSPRI-150573 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aHubbard, Alun. 245 10 ‡aHigh-resolution modeling of the advance of the Younger Dryas ice sheet and its climate in Scotland /‡cAlun Hubbard. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1999. 300 ## ‡ap. 27-43 :‡bill., diags., table. 500 ## ‡aQuaternary Research. Vol. 52(1) :27-43 (1999). 520 3# ‡aDevelops a quasi-three-dimensional, time-dependent ice flow/mass balance model for Scotland, applied at 1 km resolution. Includes essential longitudinal correction term. Reconstruction of past climatic and environmental conditions shows Scotland susceptible to glaciation after temperature depression of 2.5°C under present-day precipitation. Support is found for GRIP-style (Greenland Ice Core Project) temperature curve affecting Scotland during Younger Dryas though continued expansion under these climatic conditions conflicts with empirical evidence. 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a551.324 -- Land ice.‡2udc 650 07 ‡a551.324.4 -- Land ice, mass and energy balance.‡2udc 650 07 ‡a551.324.43 -- Land ice, regime and mass balance.‡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 ‡a551.579 -- Hydrometeorology.‡2udc 650 07 ‡a519.673 -- Modelling.‡2udc 650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local 651 #7 ‡a(411) -- Scotland.‡2udc 773 0# ‡7nnas ‡tQuaternary Research. ‡gVol. 52(1) (1999) ‡wSPRI-46567 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230925