The most rapid loss of ice from the Antarctic Ice Sheet is observed where ice streams flow
into the ocean and begin to float, forming the great Antarctic ice shelves that surround much …

Abstract The Antarctic Ice Sheet (AIS) is out of equilibrium with the current anthropogenic‐
enhanced climate forcing. Paleoenvironmental records and ice sheet models reveal that the …

Tides are a key component in coastal extreme water levels. Possible changes in the tides
caused by mean sea-level rise (SLR) are therefore of importance in the analysis of coastal …

Ocean melting has thinned Antarctica's ice shelves at an increasing rate over the past two
decades, leading to loss of grounded ice. The Ross Ice Shelf is currently close to steady …

Ocean tides are the main source of high‐frequency variability in the vertical and horizontal
motion of ice sheets near their marine margins. Floating ice shelves, which occupy about …

The circulation in a glacial fjord driven by a large tidewater glacier is investigated using a
nonhydrostatic ocean general circulation model with a melt rate parameterization at 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 …

The basal mass balance of the Amery Ice Shelf (AIS) in East Antarctica is investigated using
a numerical ocean model. The main improvements of this model over previous studies are …

Abstract We have constructed 23‐year (1994–2016) time series of Antarctic Peninsula (AP)
ice‐shelf height change using data from four satellite radar altimeters (ERS‐1, ERS‐2 …

The processes responsible for freshwater flux from the Antarctic Ice Sheet (AIS), ice‐shelf
basal melting and iceberg calving, are generally poorly represented in current Earth System …