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[PDF] Top 20 The effect of climate forcing on numerical simulations of the Cordilleran ice sheet at the Last Glacial Maximum

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The effect of climate forcing on numerical simulations of the Cordilleran ice sheet at the Last Glacial Maximum

The effect of climate forcing on numerical simulations of the Cordilleran ice sheet at the Last Glacial Maximum

... The Cordilleran ice sheet ...in climate. From a numerical modelling perspective, it is one of the least studied palaeo-ice-sheets of the Northern Hemisphere, despite the fact ... See full document

17

Numerical simulations of the Cordilleran ice sheet through the last glacial cycle

Numerical simulations of the Cordilleran ice sheet through the last glacial cycle

... the Cordilleran ice sheet of North America remains among the least understood in terms of its former extent, volume, and ...the ice sheet formed, geological studies have often had only ... See full document

26

Quantifying the effect of vegetation dynamics on the climate of the Last Glacial Maximum

Quantifying the effect of vegetation dynamics on the climate of the Last Glacial Maximum

... As shown in Ganopolski and Rahmstorf (2001), the bi- furcation transition between cold and warm modes occurs in the domain of negative anomalous freshwater forcing for the full glacial conditions. However, ... See full document

7

A new coupled ice sheet/climate model: description and sensitivity to model physics under Eemian, Last Glacial Maximum, late Holocene and modern climate conditions

A new coupled ice sheet/climate model: description and sensitivity to model physics under Eemian, Last Glacial Maximum, late Holocene and modern climate conditions

... thermal forcing, which was not resolved here as a coupled connection between ice and ocean, as the remaining mechanism available for driving Eemian AIS re- ...Antarctic ice shelf drafts) between late ... See full document

20

The effect of a dynamic soil scheme on the climate of the mid-Holocene and the Last Glacial Maximum

The effect of a dynamic soil scheme on the climate of the mid-Holocene and the Last Glacial Maximum

... amplify glacial cooling. By applying an ensemble of simulations with vary- ing forcing parameters, performed by a model of interme- diate complexity, Schneider von Deimling et ...dust forcing ... See full document

20

Marine ice sheet instability and ice shelf buttressing of the Minch ice stream, Northwest Scotland

Marine ice sheet instability and ice shelf buttressing of the Minch ice stream, Northwest Scotland

... perform numerical simulations with an idealised climate forcing to isolate the effect of marine ice sheet dynamics on the MnIS in order to determine whether the ... See full document

18

Marine ice sheet instability and ice shelf buttressing of the Minch Ice Stream, northwest Scotland

Marine ice sheet instability and ice shelf buttressing of the Minch Ice Stream, northwest Scotland

... perform numerical simulations with an idealised climate forcing to isolate the effect of marine ice sheet dynamics on the MnIS in order to determine whether the ... See full document

17

Responses of basal melting of Antarctic ice shelves to the climatic forcing of the last glacial maximum and CO2 doubling

Responses of basal melting of Antarctic ice shelves to the climatic forcing of the last glacial maximum and CO2 doubling

... Antarctic ice sheet and thinning of the ice shelves (Pritchard et ...Antarctic ice sheet under climatic conditions both warmer and colder than the present, represented by the ... See full document

25

Assessing the impact of Laurentide Ice Sheet topography on glacial climate

Assessing the impact of Laurentide Ice Sheet topography on glacial climate

... Abstract. Simulations of past climates require altered boundary conditions to account for known shifts in the Earth ...the Last Glacial Maximum (LGM) and subse- quent deglaciation, the ... See full document

21

Ice-sheet configuration in the CMIP5/PMIP3 Last Glacial Maximum experiments

Ice-sheet configuration in the CMIP5/PMIP3 Last Glacial Maximum experiments

... in forcing (Braconnot et ...simulated climate re- sponses (Schmidt et ...future climate projections and to explore the po- tential causes of inter-model spread in these ...The Last ... See full document

17

Dynamic Antarctic ice sheet during the early to mid-Miocene.

Dynamic Antarctic ice sheet during the early to mid-Miocene.

... Antarctic ice sheet had stabilized by 14 Ma [ 35], implying that the majority of glacial erosion had already occurred by this time [ 64] and that the bedrock topography may have been similar to ... See full document

7

The Effect of the Thickness-to-Die Diameter Ratio on the Sheet Metal Blanking Process

The Effect of the Thickness-to-Die Diameter Ratio on the Sheet Metal Blanking Process

... It can be understood that research studies involving blanking parameters are many and cover various aspects of the procedure by experimental and FEM methods. However, it was realized that the size of a blank should also ... See full document

9

Were the Larsemann Hills ice-free through the last Glacial Maximum?

Were the Larsemann Hills ice-free through the last Glacial Maximum?

... The stratified core from Progress Lake has a Pleistocene sediment (all dates in excess of the radiocarbon method) overlain by a dateable consistent Holocene sequence with bio[r] ... See full document

15

Usage of the yield curve in numerical simulations

Usage of the yield curve in numerical simulations

... Features o f both approaches are examined in the tensile test and deep drawing simulations. In the tensile test simulation the inverse identification method proved to be superior over Ludwig ’s law. The deep ... See full document

9

Coupling of climate models and ice sheet models by surface mass balance gradients: application to the Greenland Ice Sheet

Coupling of climate models and ice sheet models by surface mass balance gradients: application to the Greenland Ice Sheet

... coupled ice sheet-climate model system, but such a coupling set-up is still not feasi- ble due to the length of the required model simulations (kyr): ice sheet model experiments ... See full document

18

Modelling the Early Weichselian Eurasian Ice Sheets: role of ice shelves and influence of ice-dammed lakes

Modelling the Early Weichselian Eurasian Ice Sheets: role of ice shelves and influence of ice-dammed lakes

... huge ice sheet, in agreement with the QUEEN reconstruction (Svendsen et ...between simulations LA and NL is mainly due to reduced ablation on the southern flanks of the ice ...this ... See full document

12

The impact of the North American glacial topography on the evolution of the Eurasian ice sheet over the last glacial cycle

The impact of the North American glacial topography on the evolution of the Eurasian ice sheet over the last glacial cycle

... Laurentide ice sheet and the orientation of the Atlantic storm track sug- gests that the North American glacial topography may have influenced the ice-sheet evolution in ...remote ... See full document

17

The importance of snow albedo for ice sheet evolution over the last glacial cycle

The importance of snow albedo for ice sheet evolution over the last glacial cycle

... simulated ice volume evolution over the last glacial cycle ...darkening effect of dust on snow albedo than the standard scheme used in CLIMBER-2 ...excessive ice growth with an LGM ... See full document

11

The Experimental Investigation of Effects of Multiple Parameters on the Formability of the DC01 Sheet Metal

The Experimental Investigation of Effects of Multiple Parameters on the Formability of the DC01 Sheet Metal

... and numerical research ...a numerical method, Volk et ...the effect of sheet metal surface roughness, lubricant conditions and sample orientation on the value of the friction coefficient in ... See full document

12

Modeling Mediterranean Ocean climate of the Last Glacial Maximum

Modeling Mediterranean Ocean climate of the Last Glacial Maximum

... construction of LGM sea surface temperature (SST) from assemblages of foraminifera in the Mediterranean (Thiede, 1978) showed a marked difference in the cooling between eastern and western Mediterranean: the cooling in ... See full document

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