| We maintain the Parallel Ice Sheet
Model
(PISM), which simulates the thickness,
temperature, velocity and age of ice
sheets. New techniques for fast ice dynamics, earth deformation,
and
verification have been developed and included in PISM. Simulations have used up to 500
processors on computers at the
Arctic Region
Supercomputing
Center
on the UAF campus. The major purpose is to simulate the Antarctic and Greenland ice sheets over time scales of complete ice-age cycles (100,000+ years), and over the next few centuries. Such simulations are the basis of estimates of eustatic and relative sea-level changes caused by ice dynamical response to changing climate. Students involved in this effort will work with a broad range of problems in the flow of the polar ice sheets and their interactions with the oceans, the climate, and the solid earth. Students will apply modern high performance computing techniques and recent mathematical advances. Figures at right, clockwise from upper left:
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