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Evaluating an accelerated forcing approach for improving computational efficiency in coupled ice sheet–ocean modelling Geoscientific Model Development, 2024 (Ref: 17292)
Authors:
Zhou Q.Zhao C.Gladstone R.Hattermann T.Gwyther D.Galton-Fenzi B.K.
Category 1: Peer-reviewed literature

Coupled ice sheet–ocean models are increasingly being developed and applied to important questions pertaining to processes at the Greenland and Antarctic Ice Sheet margins, which play a pivotal role in ice sheet stability and sea level rise projections.

The Southern Ocean Freshwater Input from Antarctica (SOFIA) Initiative: scientific objectives and experimental design. Geoscientific Model Development, 2023 (Ref: 17137)
Authors:
Swart N.C.Martin T.Beadling R.Chen J.J.Danek C.England M.H.Farneti R.Griffies S.M.Hattermann T.Hauck J.Haumann F.A.Juling A.Li Q.Marshall J.Muilwijk M.Pauling A.G.Purich A.Smith I.J.Thomas M.
Category 1: Peer-reviewed literature

As the climate warms, the grounded ice sheet and floating ice shelves surrounding Antarctica are melting and releasing additional freshwater into the Southern Ocean. Nonetheless…

Reduced Deep Convection and Bottom Water Formation Due To Antarctic Meltwater in a Multi-Model Ensemble. Geophysical Research Letters, 2023 (Ref: 17125)
Authors:
Chen J.J.Swart N.C.Beadling R.Cheng X.Hattermann T.Juling A.Li Q.Marshall J.Martin T.Muilwijk M.Pauling A.G.Purich A.Smith I.J.Thomas M.
Category 1: Peer-reviewed literature

The additional water from the Antarctic ice sheet and ice shelves due to climate-induced melt can impact ocean circulation and global climate. However, the major processes driving melt are not adequately represented in Coupled Model Intercomparison Project phase 6 (CMIP6) models. Here…

Warming beneath an East Antarctic ice shelf due to increased subpolar westerlies and reduced sea ice. Nature Geoscience, 2023 (Ref: 17114)
Authors:
Lauber J.Hattermann T.de Steur L.Darelius E.Auger M.Nost O.A.Moholdt G.
Category 1: Peer-reviewed literature

Understanding how climate change influences ocean-driven melting of the Antarctic ice shelves is one of the greatest challenges for projecting future sea level rise. The East Antarctic ice shelf cavities host cold water masses that limit melting…

The Framework For Ice Sheet–Ocean Coupling (FISOC) V1.1 Geoscientific Model Development, 2021 (Ref: 16723)
Authors:
Gladstone R.Galton-Fenzi B.K.Gwyther D.Zhou Q.Hattermann T.Zhao C.Jong L.M.
Category 1: Peer-reviewed literature

Evaluation of an emergent feature of sub-shelf melt oscillations from an idealized coupled ice sheet–ocean model using FISOC (v1.1) – ROMSIceShelf (v1.0) – Elmer/Ice (v9.0) Geoscientific Model Development, 2022 (Ref: 16670)
Authors:
Zhao C.Gladstone R.Galton-Fenzi B.K.Gwyther D.Hattermann T.
Category 1: Peer-reviewed literature

Ocean circulation and basal melting below the Fimbul Ice Shelf, Antarctica. 26th International Forum for Research into Ice Shelf Processes (FRISP), Uto, Sweden, 12-14 June 2012, 2012 (Ref: 14965)
Authors:
Hattermann T.Nost O.A.Smedsrud L.H.Galton-Fenzi B.Lilly J.M.
Category 3: Verbal presentation

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