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A thicker Antarctic ice stream during the mid-Pliocene warm period. Communications Earth and Environment, 2023 (Ref: 17132)
Category 1: Peer-reviewed literature

Ice streams regulate most ice mass loss in Antarctica. Determining ice stream response to warmer conditions during the Pliocene could provide insights into their future behaviour, but this is hindered by a poor representation of subglacial topography in ice-sheet models.

Antarctic Wide Subglacial Hydrology Modeling Quaternary Science Reviews, 2024 (Ref: 17247)
Category 1: Peer-reviewed literature

Global sea levels are rising due, in large part, to the increase in the rate of melting of ice sheets as a direct result of climate change. A large fraction of uncertainty in future sea level rise comes from limited understanding of basal conditions under ice sheets. Specifically…

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