The thickness and equivalent global sea level contribution of an improved model of the central and northern Laurentide Ice Sheet is constrained by 24 relative sea level histories and 18 present-day GPS-measured vertical land motion rates. The final model, termed Laur16, is derived from the ICE-5G model by holding the timing history constant and iteratively adjusting the thickness history, in four regions of northern Canada. In the final model, the last glacial maximum (LGM) thickness of the Laurentide Ice Sheet west of Hudson Bay was ~3.4-3.6 km. Conversely, east of Hudson Bay, peak ice thicknesses reached ~4 km. The ice model thicknesses inferred for these two regions represent, respectively, a ~30 per cent decrease and an average ~20-25 p...
In this study we compare a recent reconstruction of the Weichselian Ice Sheet as simulated by the Un...
The last interglacial (MIS 5e) was a period characterized by sea level that was up to 6-9 m above pr...
We use a thermo-mechanically coupled ice sheet model to simulate the advance and retreat of thenorth...
The thickness and equivalent global sea level contribution of an improved model of the central and n...
We provide a global 0.5-degree grid of vertical land motion (in mm/a) of the LM17.3 glacial isostati...
Geomorphological descriptions of changes in the extent of the Greenland Ice Sheet (GIS) have been co...
[1] Motions of three hundred and sixty Global Positioning System (GPS) sites in Canada and the Unite...
The Glacial Isostatic Adjustment (GIA) process describes the response of the Earth's surface to vari...
Motions of three hundred and sixty Global Positioning System (GPS) sites in Canada and the United St...
We present a new three-dimensional thermomechanically coupled ice sheet model of the northern hemisp...
The 3D geometrical evolution of the Barents Sea Ice Sheet (BSIS), particularly during its late-glaci...
While contributing <1 m equivalent eustatic sea-level rise the British Isles ice sheet produced glac...
The 3D geometrical evolution of the Barents Sea Ice Sheet (BSIS), particularly during its late-glaci...
G44A: Cryosphere, Solid Earth, and Sea-Level Interactions and the Next Generation of Glacial Isostat...
A coupled ice sheet—ice shelf—bedrock model was run at 20km resolution to simulate the evolution of ...
In this study we compare a recent reconstruction of the Weichselian Ice Sheet as simulated by the Un...
The last interglacial (MIS 5e) was a period characterized by sea level that was up to 6-9 m above pr...
We use a thermo-mechanically coupled ice sheet model to simulate the advance and retreat of thenorth...
The thickness and equivalent global sea level contribution of an improved model of the central and n...
We provide a global 0.5-degree grid of vertical land motion (in mm/a) of the LM17.3 glacial isostati...
Geomorphological descriptions of changes in the extent of the Greenland Ice Sheet (GIS) have been co...
[1] Motions of three hundred and sixty Global Positioning System (GPS) sites in Canada and the Unite...
The Glacial Isostatic Adjustment (GIA) process describes the response of the Earth's surface to vari...
Motions of three hundred and sixty Global Positioning System (GPS) sites in Canada and the United St...
We present a new three-dimensional thermomechanically coupled ice sheet model of the northern hemisp...
The 3D geometrical evolution of the Barents Sea Ice Sheet (BSIS), particularly during its late-glaci...
While contributing <1 m equivalent eustatic sea-level rise the British Isles ice sheet produced glac...
The 3D geometrical evolution of the Barents Sea Ice Sheet (BSIS), particularly during its late-glaci...
G44A: Cryosphere, Solid Earth, and Sea-Level Interactions and the Next Generation of Glacial Isostat...
A coupled ice sheet—ice shelf—bedrock model was run at 20km resolution to simulate the evolution of ...
In this study we compare a recent reconstruction of the Weichselian Ice Sheet as simulated by the Un...
The last interglacial (MIS 5e) was a period characterized by sea level that was up to 6-9 m above pr...
We use a thermo-mechanically coupled ice sheet model to simulate the advance and retreat of thenorth...