We revisit the challenges and prospects for ocean circulation models following Griffies et al..
Over the past decade, ocean circulation models evolved through improved understanding …

Even if anthropogenic warming were constrained to less than 2° C above pre-industrial, the
Greenland and Antarctic ice sheets will continue to lose mass this century, with rates similar …

Working Group I (WGI) of the Intergovernmental Panel on Climate Change (IPCC) assesses
the current evidence on the physical science of climate change, evaluating knowledge …

Ice flow models of the Antarctic ice sheet are commonly used to simulate its future evolution
in response to different climate scenarios and inform on the mass loss that would contribute …

A potentially irreversible threshold in Antarctic ice shelf melting would be crossed if the
ocean cavity beneath the large Filchner–Ronne Ice Shelf were to become flooded with warm …

Rapid ice loss is occurring in the Amundsen Sea sector of the West Antarctic Ice Sheet. This
ice loss is assumed to be a long‐term response to oceanographic forcing, but ocean …

Climate model projections have previously been used to compute ice shelf basal melt rates
in ice sheet models, but the strategies employed–eg, ocean input, parameterization …

The ice sheet model intercomparison project for CMIP6 (ISMIP6) effort brings together the
ice sheet and climate modeling communities to gain understanding of the ice sheet …

Supported by the US Department of Energy (DOE), the Energy Exascale Earth System
Model (E3SM) project aims to optimize the use of DOE resources to address the grand …

Ice sheet numerical modeling is an important tool to estimate the dynamic contribution of the
Antarctic ice sheet to sea level rise over the coming centuries. The influence of initial …