Documentation for PISM, a parallel Ice Sheet Model

The Parallel Ice Sheet Model stable0.5 is an open source, parallel, high-resolution ice sheet model:

  • hierarchy of available stress balances
  • marine ice sheet physics, dynamic calving fronts
  • polythermal, enthalpy-based conservation of energy scheme
  • extensible coupling to atmospheric and ocean models
  • verification and validation tools
  • complete documentation for users and developers
  • uses MPI and PETSc for parallel simulations
  • reads and writes CF 1.4-compliant NetCDF

Latest News

Continued NASA funding supports PISM development through 2017

 www.nasa.gov

We have been notified that two PISM-supporting NASA research proposals have been selected for funding, one in the Cryospheric Sciences program and one in the Modeling, Analysis, and Prediction (MAP) program. Our proposed research threads focus on the dynamics of the Greenland ice sheet and on the exploitation of NASA remote observations as constraints. The current MAP grant expires in the next few months, so this news is timely. The new grants support PISM development and application for four years, through mid-2017. They include support for UAF researchers Ed Bueler, Andy Aschwanden, and Mark Fahnestock, and full-time support for scientific programmer Constantine Khroulev.

2013/03/04 20:26 · Ed Bueler

PISM Application of the Month

June 2013

Click the image to get the PDF (17.5 MB).

Changing basal conditions during the speed-up of Jakobshavn Isbræ, Greenland
investigators: Marijke Habermann, Martin Truffer, and David Maxwell, University of Alaska Fairbanks
conference: EGU 2013

Here, basal conditions for different years before and after the break-up of the tongue are inferred from surface velocity measurements to investigate the changes and to compare them with parameterizations of basal conditions commonly used in ice-sheet models.

All inversions reproduce the overall pattern of observed surface velocities, which shows that, in general, our data and model choices are capable of reproducing the observations by only adjusting basal yield stress. In the lower 5 km of the glacier a clear trend from higher to lower basal yield stress values is visible.

2013/06/03 12:53 · Andy Aschwanden

PISM team

home.txt · Last modified: 2013/03/06 09:26 by Ed Bueler
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