The sensitivity of the Antarctic ice sheet to a changing climate: Past, present, and future
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 …
enhanced climate forcing. Paleoenvironmental records and ice sheet models reveal that the …
[HTML][HTML] Antarctic ice rises and rumples: Their properties and significance for ice-sheet dynamics and evolution
Locally grounded features in ice shelves, called ice rises and rumples, play a key role
buttressing discharge from the Antarctic Ice Sheet and regulating its contribution to sea level …
buttressing discharge from the Antarctic Ice Sheet and regulating its contribution to sea level …
West Antarctic ice loss influenced by internal climate variability and anthropogenic forcing
Recent ice loss from the West Antarctic Ice Sheet has been caused by ocean melting of ice
shelves in the Amundsen Sea. Eastward wind anomalies at the shelf break enhance the …
shelves in the Amundsen Sea. Eastward wind anomalies at the shelf break enhance the …
[HTML][HTML] A protocol for calculating basal melt rates in the ISMIP6 Antarctic ice sheet projections
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 …
in ice sheet models, but the strategies employed–eg, ocean input, parameterization …
Recent irreversible retreat phase of Pine Island Glacier
Abstract Pine Island Glacier (PIG), a part of the West Antarctic marine ice sheet, has recently
undergone substantial changes including speed up, retreat and thinning. Theoretical …
undergone substantial changes including speed up, retreat and thinning. Theoretical …
Decadal ocean forcing and Antarctic ice sheet response: Lessons from the Amundsen Sea
Mass loss from the Antarctic Ice Sheet is driven by changes at the marine margins. In the
Amundsen Sea, thinning of the ice shelves has allowed the outlet glaciers to accelerate and …
Amundsen Sea, thinning of the ice shelves has allowed the outlet glaciers to accelerate and …
Anthropogenic and internal drivers of wind changes over the Amundsen Sea, West Antarctica, during the 20th and 21st centuries
Ocean-driven ice loss from the West Antarctic Ice Sheet is a significant contributor to sea-
level rise. Recent ocean variability in the Amundsen Sea sector is primarily controlled by …
level rise. Recent ocean variability in the Amundsen Sea sector is primarily controlled by …
The influence of Pine Island Ice Shelf calving on basal melting
The combination of the Pine Island Ice Shelf (PIIS) draft and a seabed ridge beneath it form
a topographic barrier, restricting access of warm Circumpolar Deep Water to a cavity inshore …
a topographic barrier, restricting access of warm Circumpolar Deep Water to a cavity inshore …
Experimental design for three interrelated marine ice sheet and ocean model intercomparison projects: MISMIP v. 3 (MISMIP+), ISOMIP v. 2 (ISOMIP+) and MISOMIP v …
Coupled ice sheet–ocean models capable of simulating moving grounding lines are just
becoming available. Such models have a broad range of potential applications in studying …
becoming available. Such models have a broad range of potential applications in studying …
Strong ocean melting feedback during the recent retreat of Thwaites Glacier
Accelerating ice loss from Thwaites Glacier is contributing approximately 5% of global sea‐
level rise, and could add tens of centimeters to sea level over the coming centuries. We use …
level rise, and could add tens of centimeters to sea level over the coming centuries. We use …