Ice sheet dynamics describe the motion within large bodies of ice, such those currently on Greenland and Antarctica. Ice motion is dominated by the movement of glaciers, whose gravity-driven activity is controlled by two main variable factors: the temperature and strength of their bases. A number of processes alter these two factors, resulting in cyclic surges of activity interspersed with longer periods of inactivity, on both hourly and centennial time scales.
Read more about Ice Sheet Dynamics: Flow Dynamics, Glacial Bottom Processes, Erosional Effects, Pipe and Sheet Flow, Boundary Conditions, Long-term Changes, Effects of Climate Change On Ice Sheet Dynamics
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