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Titlebook: Ice in the Climate System; W. Richard Peltier Conference proceedings 1993 Springer-Verlag Berlin Heidelberg 1993 Eis.Orbit.Scale.Snow.Tide

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Ice, Climate, and Sea Level; Do We Know What is Happening?9), Oerlemans (1989), Meier (1990b), Warrick and Oerlemans (1990), Budd and Simmonds (1991), and Schneider (1992). How confident can these predictions be, given our incomplete knowledge of the present condition?
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The driving force of brine rejection on the deepwater formation in the Hamburg LSG OGCMr falls below the freezing point by more than a few tens of centigrades. With the incorporation of a sea ice model the OGCM can react on prescribed atmospheric temperatures which fall below −30 °C. The problem of a warming deep ocean then vanishes.
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Climate Model Studies of Interactions between Ice Sheets and the Atmosphere-Ocean Systemlimate, although questions regarding the refreezing of surface meltwater make this result uncertain. Results from climate model experiments with and without orography suggest that orographic uplift could have produced a climate slightly more favorable for ice sheet initiation.
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Controls on Changes in the West Antarctic Ice SheetThe West Antarctic Ice Sheet is changing now. The cause for these changes lies with the mechanical controls on the flow of ice streams. These controls are associated with basal friction and with lateral drag. The ice sheet is changing largely independently of forcings by global sea level and climate, and is rather a forcing for sea level.
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Plastic Modelling of Glaciers and Outlets basic in the model has been that the bottom shear stress is assumed constant along a flowline (Orowan, 1949). This gives a simple calculation scheme for an ice sheet profile with an arbitrary bed surface. The unit “force” that cause this bottom shear stress is popularly called “driving stress”.
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https://doi.org/10.1007/978-3-642-85016-5Eis; Orbit; Scale; Snow; Tide; atmosphere; carbon dioxide; climate; climate change; environment; ocean; oceanog
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