GREB-ISM

The Globally Resolved Energy Balance – Ice Sheet Model v1.0 (GREB-ISM v1.0) (Xie et al., 2022) is a fully coupled global ice-sheet–climate modeling system capable of simulating the evolution of grounded ice sheets and floating ice shelves on a global grid. The model explicitly accounts for interactions with key climate components, including surface temperature, snowfall, albedo, land–sea distribution, topography, and sea level.

Schematic of the thermal slope effect of ice sheets
GREB-ISM coupling diagram

GREB-ISM is integrated with the Globally Resolved Energy Balance climate model v2.0 (GREB v2.0) (Dommenget & Flöter, 2011; Stassen et al., 2019), which represents the climate system using three physical layers — atmosphere, surface, and deep ocean — at a horizontal resolution of 3.75° × 3.75° (96 × 48 grid points). The GREB model also includes a simplified treatment of atmospheric water vapor based on evaporation, precipitation, and atmospheric transport. Precipitation is determined diagnostically following Stassen et al. (2019). Since GREB-ISM is a fast and efficient model, it is a suitable tool for paleoclimate simulation.

The ice-sheet module of GREB-ISM is a three-dimensional model with four vertical layers, using the shallow-ice approximation (SIA) for grounded ice and the shallow-shelf approximation (SSA) with constant viscosity for floating ice shelves. Surface melt rates are computed from the surface energy balance provided by GREB v2.0. Together, these components enable GREB-ISM to efficiently simulate long-timescale ice-sheet evolution and climate feedbacks on global scales.

Schematic of the thermal slope effect of ice sheets
GREB-ISM ice sheet model diagram

References