Hydrography, circulation, and response to atmospheric forcing in the vicinity of the central Getz Ice Shelf, Amundsen Sea, Antarctica

• Published in: Ocean Science
• Main Authors: V. Dundas, E. Darelius, K. Daae, N. Steiger, Y. Nakayama, T.-W. Kim
• Format: Article in Journal/Newspaper
• Language: English
• Published: Copernicus Publications 2022
• Subjects: Geography. Anthropology. Recreation; G; Environmental sciences; GE1-350; Amundsen Sea; Siple; Getz; Getz Ice Shelf; Carney Island; Antarc*; Antarctica; Ice Shelf; Ice Shelves; Sea ice
• Online Access: https://doi.org/10.5194/os-18-1339-2022; https://doaj.org/article/64413c1f6eab49d5adc7fc5b18d52d11

Ice shelves in the Amundsen Sea are thinning rapidly as ocean currents bring warm water into the cavities beneath the floating ice. Although the reported melt rates for the Getz Ice Shelf are comparatively low for the region, its size makes it one of the largest freshwater sources around Antarctica, with potential consequences for, bottom water formation downstream, for example. Here, we use a 2-year-long novel mooring record (2016–2018) and 16-year-long regional model simulations to describe, for the first time, the hydrography and circulation in the vicinity of the ice front between Siple and Carney Island. We find that, throughout the mooring record, temperatures in the trough remain below 0.15 ∘ C, more than 1 ∘ C lower than in the neighboring Siple and Dotson Trough, and we observe a mean current (0.03 m s −1 ) directed toward the ice shelf front. The variability in the heat transport toward the ice shelf appears to be governed by nonlocal ocean surface stress over the Amundsen Sea Polynya region, and northward to the continental shelf break, where strengthened westward ocean surface stress leads to increased southward flow at the mooring site. The model simulations suggest that the heat content in the trough during the observed period was lower than normal, possibly owing to anomalously low summertime sea ice concentration and weak winds.