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Antarctic densewater formation sensitivity to ocean surface cell thickness. Journal of Advances in Modeling Earth Systems, 2025 (Ref: 17452)
Category 1: Peer-reviewed literature

Dense water formation on the Antarctic continental shelf is the main process by which Antarctic Bottom Waters form and is fundamental to the abyssal overturning circulation. However…

Impact of anthropogenic climate change on Antarctic dense shelf water in a high-resolution Community Earth System Model (CESM1.3) Climate Dynamics, 2025 (Ref: 17432)
Category 1: Peer-reviewed literature

Dense shelf water (DSW) overflows around Antarctica leads to the formation of antarctic bottom water, thereby driving the lower cell of global overturning circulation.

Unlocking Southern Ocean Under-Ice Seasonality With a New Monthly Climatology Journal of Geophysical Research: Oceans, 2025 (Ref: 17283)
Category 1: Peer-reviewed literature

The advent of under-ice profiling float and biologging techniques has enabled year-round observation of the Southern Ocean and its Antarctic margin. These under-ice data are often overlooked in widely used oceanographic datasets…

The CSIRO-BoM-AAD Antarctic and Southern Ocean Atmospheric Composition Monitoring Network Strategic Science in Antarctica Conference, Hobart, Australia, 24-26 June 2013, 2013 (Ref: 15569)
Category 3: Poster

Gases released by human activity (greenhouse and ozone depleting gases) are responsible for global change. They are long-lived and well-mixed in the atmosphere. The Antarctic regions, remote from industrial and land plant activity are ideally located to measure global changes in the gases.

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