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Circulation and ocean–ice shelf interaction beneath the Denman and Shackleton Ice Shelves Science Advances, 2025 (Ref: 17478)
Category 1: Peer-reviewed literature

Ocean-driven basal melt can thin and weaken ice shelves, reducing buttressing and causing sea level rise. However, the processes driving melt in ice shelf cavities are challenging to observe. Here we report float observations spanning the ocean cavity beneath Shackleton Ice Shelf.

Deep Argo improves the accuracy and resolution of ocean bathymetry Earth and Space Science, 2025 (Ref: 17445)
Category 1: Peer-reviewed literature

Ocean bathymetry plays an instrumental role in stirring ocean circulation and ocean mixing, shaping the transport of ocean heat, freshwater, oxygen, and carbon, influencing the propagation of tides and tsunamis, and controlling the dispersion of sediments, nutrients, and planktonic species.

On-shelf circulation of warm water toward the Totten Ice Shelf in East Antarctica. Nature Communications, 2023 (Ref: 17117)
Category 1: Peer-reviewed literature

The Totten Glacier in East Antarctica, with an ice volume equivalent to >3.5?m of global sea-level rise, is grounded below sea level and, therefore, vulnerable to ocean forcing. Here…

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