Documentation for PISM, the Parallel Ice Sheet Model

August 2015

The Antarctic ice sheet (AIS) will likely experience higher snow accumulation rates in a warmer climate because warmer air has a higher moisture-holding capacity. This paper quantifies the effect based on ice-core data and paleo-climate simulations, which together show a consistent continental-scale accumulation increase of 5 percent per degree Kelvin. (Note ice-core data and GCM-type modelling results agree for the last deglaciation.) However, some of the mass gain of the AIS is offset by dynamical losses induced by accumulation. This is where PISM plays a supporting role in the paper. PISM results were used to generate a response function allowing projections of sea-level fall in terms of continental-scale accumulation changes. In PISM the accumulation changes can and do compete with changes in surface melting and with dynamical losses induced by mechanisms like ocean interaction and sliding.

applications/201508.txt ยท Last modified: 2015/12/10 15:31 by Ed Bueler
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