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Record #110537:
- #110537
Main publication details
MARC recordClimate model comparison of Gondwanan and Laurentide glaciations / Thomas J. Crowley, Steven K. Baum, William T. Hyde.
| Title: | Climate model comparison of Gondwanan and Laurentide glaciations / Thomas J. Crowley, Steven K. Baum, William T. Hyde. |
| Author(s): | Crowley, Thomas J. Baum, Steven K. Hyde, William T. |
| Date: | 1991. |
| In: | Journal of Geophysical Research. (1991.), Vol. 96(D5) (1991) |
| Abstract: | Focuses on major difference between boundary conditions of these two glaciations: Gondwanan glaciations occurred on large landmass, or supercontinent. Three levels of sensitivity experiments were conducted to examine effects of large landmass on magnitude of summer warming over ice sheets. Results suggest that conditions necessary to explain Gondwanan ice-sheet stability may be known, but required boundary conditions would be more extreme than in Pleistocene. |
| Notes: | Journal of Geophysical Research. Vol. 96(D5) :9217-9226 (1991). |
| Keywords: | 551.32 -- Glaciology. 551.336 -- Ice ages. 551.73 -- Palaeozoic. 551.76 -- Mesozoic. 551.79 -- Quaternary. 551.583.7 -- Palaeoclimatology. 519.673 -- Modelling. E7 -- Glaciology: glacial geology and ice ages. (217.5) -- Gondwana. (217.2) -- Laurentia. |
| SPRI record no.: | 110537 |
LDR 01541naa#a2200000#a#4500 001 SPRI-110537 005 20230330153557.0 007 ta 008 230330s1991####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-110537 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aCrowley, Thomas J. 245 10 ‡aClimate model comparison of Gondwanan and Laurentide glaciations /‡cThomas J. Crowley, Steven K. Baum, William T. Hyde. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1991. 300 ## ‡ap. 9217-9226 :‡bdiags., maps. 500 ## ‡aJournal of Geophysical Research. Vol. 96(D5) :9217-9226 (1991). 520 3# ‡aFocuses on major difference between boundary conditions of these two glaciations: Gondwanan glaciations occurred on large landmass, or supercontinent. Three levels of sensitivity experiments were conducted to examine effects of large landmass on magnitude of summer warming over ice sheets. Results suggest that conditions necessary to explain Gondwanan ice-sheet stability may be known, but required boundary conditions would be more extreme than in Pleistocene. 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a551.336 -- Ice ages.‡2udc 650 07 ‡a551.73 -- Palaeozoic.‡2udc 650 07 ‡a551.76 -- Mesozoic.‡2udc 650 07 ‡a551.79 -- Quaternary.‡2udc 650 07 ‡a551.583.7 -- Palaeoclimatology.‡2udc 650 07 ‡a519.673 -- Modelling.‡2udc 650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local 651 #7 ‡a(217.5) -- Gondwana.‡2udc 651 #7 ‡a(217.2) -- Laurentia.‡2udc 700 1# ‡aBaum, Steven K. 700 1# ‡aHyde, William T. 773 0# ‡7nnas ‡tJournal of Geophysical Research. ‡gVol. 96(D5) (1991) ‡wSPRI-35252 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230330