Multistability of the Greenland ice sheet and the effects of an adaptive mass balance formulation

Published: Jul 1, 2012 by The PISM Authors

   
Title Multistability of the Greenland ice sheet and the effects of an adaptive mass balance formulation
Authors Anne M. Solgaard and Peter L. Langen
Venue Climate Dynamics
Location Greenland

We use output from a general circulation model (CAM3+CLM) to construct adaptive temperature and precipitation patterns to force PISM off-line, taking into consideration that the patterns change in a non-uniform way, both spatially and temporally, as the geometry of the ice sheet evolves and as climate changes. In a series of experiments we investigate retreat from the present day configuration and build-up from ice free conditions during a warmer-than-present climate. We find that the ice sheet is able to survive and build up at higher temperatures using the more realistic adaptive patterns compared to the classic constant patterns. The ice sheet is multistable at least for certain temperature forcings, so it does not necessarily return to its initial configuration after a temperature excursion.

Share

Latest news

PISM 2.2.1 is out

We are pleased to announce the release of PISM v2.2.1.

Scientist for Modeling Ice Sheet–Climate Interaction at DMI

The Danish Meteorological Institute (DMI), a leading research institution in climate and ice sheet modelling research, is offering a 3-year, full-time position as a Scientist for Modelling Ice Sheet–Climate Interaction.

MPI-GEA: PhD position on the interaction of ice sheets, ocean and sea level

In the department of Integrative Earth system science at the newly founded Max Planck Institute of Geoanthropology (MPI-GEA) in Jena, Germany, we are providing a three-year PhD position as part of the DFG priority program “Antarctic Research with Comparative Investigations in Arctic Ice Areas”.