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Reduced Deep Convection and Bottom Water Formation Due To Antarctic Meltwater in a Multi-Model Ensemble. Geophysical Research Letters, 2023 (Ref: 17125)
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…

Return of the Maud Rise Polynya: Climate litmus or sea ice anomaly? [In: State of the Climate in 2017] Bulletin of the American Meteorological Society, 2018 (Ref: 17043)
Category 1: Peer-reviewed literature

The Maud Rise polynya is a persistent area of open water within the sea ice cover of the Southern Ocean, which overlies an area of elevated topography called Maud Rise (66°S, 3°E) located in the eastern sector of the Weddell Sea (Fig. SB6.1a).

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