Bedforms of Thwaites Glacier, West Antarctica: Character and Origin [PDF]
Bedforms of Thwaites Glacier, West Antarctica both record and affect ice flow, as shown by geophysical data and simple models. Thwaites Glacier flows across the tectonic fabric of the West Antarctic rift system with its bedrock highs and sedimentary ...
Nathan Stevens +2 more
exaly +11 more sources
Brief communication: Thwaites Glacier cavity evolution [PDF]
Between 2014 and 2017, ocean melt eroded a large cavity beneath and along the western margin of the fast-flowing core of Thwaites Glacier. Here we show that from 2017 to the end of 2020 the cavity persisted but did not expand.
S. L. Bevan +4 more
doaj +9 more sources
Heterogeneous retreat and ice melt of Thwaites Glacier, West Antarctica. [PDF]
The heterogeneous retreat of Thwaites glacier indicates complexities of ice melt processes taking place at the grounding zone. The glaciers flowing into the Amundsen Sea Embayment, West Antarctica, have undergone acceleration and grounding line retreat ...
Milillo P +6 more
europepmc +9 more sources
Geological sketch map and implications for ice flow of Thwaites Glacier, West Antarctica, from integrated aerogeophysical observations. [PDF]
The geology beneath Thwaites Glacier, the Antarctic glacial catchment most vulnerable to climate change, is unknown. Thwaites Glacier lies within the West Antarctic Rift System, but details of the subglacial geology relevant to glacial flow, including ...
Jordan TA +3 more
europepmc +6 more sources
Sedimentary Signatures of Persistent Subglacial Meltwater Drainage From Thwaites Glacier, Antarctica [PDF]
Subglacial meltwater drainage can enhance localized melting along grounding zones and beneath the ice shelves of marine-terminating glaciers. Efforts to constrain the evolution of subglacial hydrology and the resulting influence on ice stability in space
A. P. Lepp +13 more
doaj +3 more sources
Intermittent structural weakening and acceleration of the Thwaites Glacier Tongue between 2000 and 2018 [PDF]
Evolving conditions at the terminus of Thwaites Glacier will be important in determining the rate of its future sea-level contribution over the coming decades.
B. W. J. Miles +5 more
doaj +3 more sources
Weakening of the pinning point buttressing Thwaites Glacier, West Antarctica [PDF]
The Thwaites Eastern Ice Shelf buttresses a significant portion of Thwaites Glacier through contact with a pinning point 40 km offshore of the present grounding line. Predicting future rates of Thwaites Glacier’s contribution to sea-level rise depends on
C. T. Wild +5 more
doaj +4 more sources
Mass Loss From Thwaites Glacier Continues Even Without Ocean Melting
Pine Island and Thwaites glaciers dominate Antarctica's sea‐level contribution. However, it remains unclear whether their ice loss is driven by anomalously warm present‐day ocean conditions, perhaps linked to anthropogenic climate change, or are an ...
C. Rosie Williams +6 more
doaj +3 more sources
Derivation of bedrock topography measurement requirements for the reduction of uncertainty in ice-sheet model projections of Thwaites Glacier [PDF]
Determining the future evolution of the Antarctic Ice Sheet is critical for understanding and narrowing the large existing uncertainties in century-scale global mean sea-level-rise (SLR) projections.
B. A. Castleman +5 more
doaj +2 more sources
Widespread seawater intrusions beneath the grounded ice of Thwaites Glacier, West Antarctica. [PDF]
Significance We present evidence for seawater intrusions occurring at tidal frequencies over many kilometers beneath the grounded ice of Thwaites Glacier, West Antarctica, a major contributor to sea level rise.
Rignot E +5 more
europepmc +2 more sources

