Throughout the latter half of the Pleistocene epoch of Earth history, beginning∼ 900 kyr ago,
the climate system has been dominated by an intense oscillation between full glacial and …

This paper models the extent of the Patagonian icesheet during the Last Glacial Maximum
(LGM) and its subsequent deglaciation. It constrains a new coupled icesheet/climate …

This report is the first complete assessment of the science of climate change since Working
Group I (WGI) of the IPCC produced its second report Climate Change 1995: The Science of …

Glaciers and Glaciation is the classic textbook for all students of glaciation. Stimulating and
accessible, it has established a reputation as a comprehensive and essential resource. In …

The ice sheet–ice shelf transition zone plays an important role in controlling marine ice
sheet dynamics, as it determines the rate at which ice flows out of the grounded part of the …

Global-scale 21st-century glacier mass change projections from six published global glacier
models are systematically compared as part of the Glacier Model Intercomparison Project. In …

Ice flow models used to project the mass balance of ice sheets in Greenland and Antarctica
usually rely on the Shallow Ice Approximation (SIA) and the Shallow‐Shelf Approximation …

Dynamics of Ice Sheets and Glaciers presents an introduction to the dynamics and
thermodynamics of flowing ice masses on Earth. Based on an outline of general continuum …

A new three‐dimensional thermomechanically coupled ice sheet model is developed.
Contrary to the majority of three‐dimensional ice sheet models (shallow ice approximation) …

The Dynamic Response of the Greenland and Antarctic Ice Sheets to Multiple-Century Climatic
Warming in: Journal of Climate Volume 12 Issue 8 (1999) Jump to Content Jump to Main …