Abstract
The contribution to sea-level rise from ice sheets is increasing. Observed acceleration in the rate of ice loss from the Greenland and Antarctic ice sheets is a concern, particularly for the West Antarctic Ice Sheet, which is largely grounded below sea level. This geometric configuration makes Antarctica susceptible to a dynamic instability that could result in a catastrophic collapse of one or more ice shelves as a result of relatively small perturbations at the ice sheet's margins. While ice sheet models have become significantly more advanced over the past decade, they are still incomplete in many ways; hence, there are large uncertainties in these models' projections of future sea-level rise. The goal of the ProSPect SciDAC partnership is to address current limitations of DOE ice sheet and Earth system models that limit their use for making accurate sea-level projections. These include inadequate or missing model physics, incomplete couplings between models, and deficiencies in methods for model initialization, validation, and uncertainty quantification. This poster focuses on recent ProSPect efforts towards ice sheet model development to incorporate missing physics (ice damage, fracture and calving, subglacial hydrology, enthalpy) and to improve the overall computational efficiency and portability of the models (through the incorporation of adaptive mesh refinement, scalable and efficient solvers preconditioners and performance portable kernels).