Antarctica is currently losing net mass to the ocean primarily from West Antarctica and the
Antarctic Peninsula, which together hold~ 5.5 m of sea level rise potential. Yet, the East …

How much Antarctic ice shelf basal melt rates can increase in response to global warming
remains an open question. Here we describe the response of the Southern Ocean and ice …

Glaciers along the Amundsen Sea coastline in West Antarctica are dynamically adjusting to
a change in ice-shelf mass balance that triggered their retreat and speed-up prior to the …

Ice sheet mass loss from Antarctica is greatest in the Amundsen Sea sector, where “warm”
modified Circumpolar Deep Water moves onto the continental shelf and melts and thins the …

Global-and basin-scale ocean reanalyses are becoming easily accessible and are utilized
widely to study the Southern Ocean. However, such ocean reanalyses are optimized to …

Abstract The Marine Ice Sheet–Ocean Model Intercomparison Project–phase 2 (MISOMIP2)
is a natural progression of previous and ongoing model intercomparison exercises that have …

Surface freshening of the Southern Ocean driven by meltwater discharge from the Antarctic
ice sheet has been shown to influence global climate dynamics. However, most climate …

Workshop on Antarctic Ice Shelf Processes in Models and Earth Observation What: The
meeting brought together 25 scientists specializing in diverse fields related to Earth …

We are in a period of rapidly accelerating change across the Antarctic continent and
Southern Ocean, with land ice loss leading to sea level rise and multiple other climate …

The integration of data from multiple satellite altimetry missions, each offering unique
observational characteristics, has enabled us to discern both short-term variability and long …