Self-inhibiting growth of the Greenland Ice Sheet

Published: Dec 1, 2012 by The PISM Authors

   
Title Self-inhibiting growth of the Greenland Ice Sheet
Authors Peter Langen and others
Venue Geophysical Research Letters

The build-up of the Greenland Ice Sheet from ice-free conditions is studied using PISM driven by fields from an atmospheric GCM. Experiments where the two are coupled off-line are augmented by one where an intermediate ice sheet configuration is coupled back to the GCM. The ice sheet regrows from the ice-free state but this is halted when the intermediate recoupling step is included. This inhibition of further growth is due to a Föhn effect of moist air parcels being lifted over the intermediate ice sheet and arriving in the low-lying Greenland interior with high temperatures. This demonstrates that two-way coupling between the atmosphere and the ice sheet is essential for understanding its dynamics. Conditions cooler than those of today may be necessary for the GrIS to regrow to the present volume.

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”.