Thwaites Glacier is one of the fastest-changing ice–ocean systems in Antarctica 1, 2, 3. Much of the ice sheet within the catchment of Thwaites Glacier is grounded below sea level …
Ocean conditions near the grounding zones of Antarctica's ice shelves play a key role in controlling the outflow and mass balance of the ice sheet. However, ocean observations in …
Thwaites Glacier is the most rapidly changing outlet of the West Antarctic Ice Sheet and adds large uncertainty to 21st century sea-level rise predictions. Here, we present the first direct …
MG Rosevear, B Gayen, CA Vreugdenhil… - Annual Review of …, 2024 - annualreviews.org
The present-day state and future of the Antarctic Ice Sheet depend on the rate at which the ocean melts its fringing ice shelves. Ocean heat must cross many physical and dynamical …
Throughout coastal Antarctica, ice shelves separate oceanic waters from sunlight by hundreds of meters of ice. Historical studies have detected activity of nitrifying …
SS Jacobs, CF Giulivi, P Dutrieux - Journal of Geophysical …, 2022 - Wiley Online Library
A 63‐year observational record in the southwest Ross Sea shows a continuing, near‐linear salinity decrease of 0.170 and slight warming of 0.013° C through 2020. That freshening …
Ice streams flowing into Ross Ice Shelf are presently responsible for around 10% of the mass flux from West Antarctica, with the noteworthy exception of Kamb Ice Stream, which …
MG Rosevear, B Gayen… - Journal of Physical …, 2022 - journals.ametsoc.org
Abstract The Antarctic Ice Sheet is losing mass as a result of increased ocean-driven melting of its fringing ice shelves. Efforts to represent the effects of basal melting in sea level …
The seafloor beneath floating ice shelves accounts roughly a third of the Antarctic's 5 million km2 of continental shelf. Prior to this study, our knowledge of these habitats and the life they …