Recent advances in both ocean modeling and melt parameterization in ice-sheet models
point the way toward coupled ice sheet–ocean modeling, which is needed to quantify …

Numerical modeling of the Antarctic ice sheet has gone through a paradigm shift over the
last decade. While initially models focussed on long-time diffusive response to surface mass …

While a lot of attention has been given to the numerical implementation of grounding lines
and basal friction in the grounding zone, little has been done about the impact of the …

Ocean-induced basal melting is responsible for much of the Amundsen Sea Embayment ice
loss in recent decades, but the total magnitude and spatiotemporal evolution of this melt is …

Ice shelves play a vital role in regulating loss of grounded ice and in supplying freshwater to
coastal seas. However, melt variability within ice shelves is poorly constrained and may be …

Assessment of ocean‐forced ice sheet loss requires that ocean models be able to represent
sub‐ice shelf melt rates. However, spatial accuracy of modeled melt is not well investigated …

Ice shelves buttress ice streams and glaciers, slowing the rate at which they flow into the
ocean. When this buttressing is reduced, either through increased melt or calving, the …

This study assesses the response on ice dynamics of Petermann Glacier, a major outlet
glacier in northern Greenland, to the 2012 and a possible future calving event. So far …

Systematic long-term studies on ecosystem dynamics are largely lacking from the East
Antarctic Southern Ocean, although it is well recognized that they are indispensable to …

Ice shelves regulate the ice‐ocean boundary by buttressing the flux of grounded ice into the
ocean and are vulnerable to basal melt, which can lead to ice‐shelf thinning and loss of …