Results 1 to 10 of about 153,318 (201)
The Impact of Basal Roughness on Inland Thwaites Glacier Sliding [PDF]
Swath radar technology enables three‐dimensional mapping of modern glacier beds over large areas at resolutions that are higher than those typically used in ice‐flow models.
Andrew O. Hoffman +5 more
doaj +8 more sources
Heterogeneous melting near the Thwaites Glacier grounding line. [PDF]
Thwaites Eastern Ice Shelf observations from a new underwater vehicle show that high melt rates occur where ice is sharply sloped at the ocean interface, with lower melt where the ice is comparatively flat.
Schmidt BE +25 more
europepmc +13 more sources
Rapid retreat of Thwaites Glacier in the pre-satellite era. [PDF]
Understanding the recent history of Thwaites Glacier, and the processes controlling its ongoing retreat, is key to projecting Antarctic contributions to future sea-level rise.
Graham AGC +11 more
europepmc +9 more sources
Suppressed basal melting in the eastern Thwaites Glacier grounding zone. [PDF]
Despite observations from a hot-water-drilled access hole showing warm ocean waters beneath Thwaites Glacier Eastern Ice Shelf, the basal melt rate is strongly suppressed due to the low current speeds and strong density stratification.
Davis PED +22 more
europepmc +11 more sources
Strong Ocean Melting Feedback During the Recent Retreat of Thwaites Glacier [PDF]
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.
Paul R Holland +2 more
exaly +6 more sources
Hard rocks and deep wetlands beneath Thwaites Glacier in Antarctica [PDF]
Thwaites Glacier in West Antarctica is losing ice rapidly and is considered especially vulnerable to retreat, but predictions of its future remain limited by uncertainties about its subglacial properties.
Ole Zeising +7 more
doaj +5 more sources
Drivers of Change of Thwaites Glacier, West Antarctica, Between 1995 and 2015 [PDF]
Using three independent ice‐flow models and several satellite‐based datasets, we assess the importance of correctly capturing ice‐shelf breakup, shelf thinning, and reduction in basal traction from ungrounding in reproducing observed speed‐up and ...
Mathieu Morlighem +2 more
exaly +5 more sources
The influence of subglacial lake discharge on Thwaites Glacier ice-shelf melting and grounding-line retreat [PDF]
The retreat of the Antarctic Ice Sheet is conventionally attributed to increased ocean melting of ice shelves, potentially enhanced by internal instability from grounding lines near retrograde bed slopes.
N. Gourmelen +7 more
doaj +3 more sources
Sea-level contribution from Thwaites Glacier doubles in an observation-constrained ice-sheet model [PDF]
Thwaites Glacier is a major contributor to Antarctic mass loss and a key source of uncertainty in future sea-level rise. Ocean-driven melting at its grounding line drives rapid retreat, yet most models treat the transition between grounded and floating ...
Mattia Poinelli +5 more
doaj +3 more sources
The Thwaites Glacier (TG), accounting for four percent of present-day sea-level rise, has been confirmed with the irreversible retreat and thinning. Consequently, understanding the continuous calving front retreat within the TG is pivotal for accurately ...
Dong Liang, Zherong Wu
exaly +4 more sources

