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Effects of Sediment-Laden Subglacial Discharge on Ice Shelf Basal Melting and Seabed Evolution Journal of Geophysical Research: Oceans, 2025 (Ref: 17473)
Category 1: Peer-reviewed literature

The grounding zone—where glaciers transition to floating ice shelves—critically influences ice sheet mass loss yet remains poorly observed. While tides and subglacial freshwater enhance basal melt, the role of sediment-laden subglacial water outflow on ice shelf–ocean dynamics is unexplored.

Investigating gravity waves in the polar atmosphere – ANGWIN past and future URSI AP-RASC conference, Sydney, Australia, 17-22 August 2025, 2025 (Ref: 17365)
Category 3: Abstract

Gravity waves provide a key mechanism for the vertical transport of energy and momentum from the active near-surface weather to the upper reaches of the neutral and ionised atmosphere. Generation mechanisms vary between storms, fronts…

Subglacial water amplifies Antarctic contributions to sea-level rise Nature Communications, 2025 (Ref: 17328)
Category 1: Peer-reviewed literature

Antarctica's contribution to global sea-level rise is deeply uncertain, with subglacial water suspected to play a critical role, yet its impact remains unclear.

Sensitivity of the future evolution of the Wilkes Subglacial Basin ice sheet to grounding-line melt parameterizations The Cryosphere, 2024 (Ref: 17204)
Category 1: Peer-reviewed literature

Projections of Antarctic Ice Sheet mass loss and therefore global sea level rise are hugely uncertain, partly due to how mass loss of the ice sheet occurs at the grounding line. The Wilkes Subglacial Basin (WSB), a vast region of the East Antarctic Ice Sheet…

Exploring grid sensitivity in an ice sheet model: A case study of the Amery Ice Shelf Advances in Climate Change Research, 2024 (Ref: 17289)
Category 1: Peer-reviewed literature

The dynamics of the Antarctic ice sheet are key factors affecting global climate change. To project future sea level changes, ice sheet models are developed based on a discrete grid system, which profoundly impacts the accuracy of numerical simulations.

Evaluating an accelerated forcing approach for improving computational efficiency in coupled ice sheet–ocean modelling Geoscientific Model Development, 2024 (Ref: 17292)
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 potential of using fishing vessels as a research platform to address knowledge gaps in krill biology for supporting krill management CCAMLR Working Group on Ecosystem Monitoring and Management, Virtual Meeting 4 to 11 July 2022, 2022 (Ref: 17012)
Category 2: International meeting papers

Here we present preliminary results on krill distribution from data collected from the Norwegian fishing vessel (F/V) Antarctic Endurance during her commercial operation for Antarctic krill in subareas 48.1 and 48.2 during different timings of the year in 2020, 2021 and 2022.

Standing stock of Antarctic krill (Euphausia superba Dana, 1850) (Euphausiacea) in the Southwest Atlantic sector of the Southern Ocean, 2018–19 Journal of Crustacean Biology, 2021 (Ref: 16595)
Category 1: Peer-reviewed literature

Estimates of the distribution and density of Antarctic krill (Euphausia superba Dana, 1850) were derived from a large-scale survey conducted during the austral summer in the Southwest Atlantic sector of the Southern Ocean and across the Scotia Sea in 2018–19, the ‘2018–19 Area 48 Survey’.

Linking timescale-dependent Antarctic sea ice kinematic observations to ice thickness Remote Sensing of Environment, 2023 (Ref: 16893)
Category 1: Peer-reviewed literature

Sea ice kinematics impacts the global ocean–atmosphere system in numerous ways: modification of albedo, ice cover, and ice mass; heat transmission between atmosphere and ocean; and ice thickness distribution.

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