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Antarctic Bottom Water in a changing climate Nature Reviews: Earth & Environment, 2025 (Ref: 17477)
Category 1: Peer-reviewed literature

Antarctic Bottom Water (AABW) is derived from dense water that sinks from the Antarctic continental shelf to the deep ocean. The sinking of AABW is balanced by a return flow of lighter water, and the resulting overturning circulation determines the density stratification of the deep ocean…

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…

Seasonal variability of ocean heat transport and ice-shelf basal melt around Antarctica The Cryosphere, 2025 (Ref: 17420)
Category 1: Peer-reviewed literature

The delivery of ocean heat to Antarctic ice shelves is due to intrusions of waters warmer than the local freezing point temperature. Changes in the supply of ocean heat will determine how rapidly ice shelves melt at their base…

The variability of Antarctic dense water overflows can be observed from space Communications, Earth and Environment, 2025 (Ref: 17347)
Category 1: Peer-reviewed literature

Around the margins of Antarctica, dense waters formed on the continental shelf are exported to oceanic depths. This overflow of dense waters to the abyss ventilates the ocean, and is vital to the global overturning circulation.

Enhancing Global Ocean Science Networks: The Impact of SCOR's Travel Grant Initiative Oceanography, 2025 (Ref: 17226)
Category 3: Article

The capacity sharing approach of the Scientific Committee on Oceanic Research (SCOR) focuses on supporting opportunities for individual ocean scientists and students within SCOR's portfolio of scientific activities and through targeted capacity development opportunities (Morrison et al.…

Environmental drivers of tropospheric bromine and mercury variability in coastal East Antarctica Atmospheric Environment, 2024 (Ref: 17202)
Category 1: Peer-reviewed literature

Bromine radicals released from sea ice, snow, and marine sources play a critical role in the atmospheric chemistry of polar regions. The Chemical and Mesoscale Mechanisms of Polar Cell Aerosol Nucleation (CAMMPCAN)…

Decoupling of the Surface and Bottom?Intensified Antarctic Slope Current in Regions of Dense Shelf Water Export. Geophysical Research Letters, 2023 (Ref: 17116)
Category 1: Peer-reviewed literature

The Antarctic Slope Current is guided by the topographic gradient of the Antarctic continental slope and creates a dynamical barrier between the continental shelf and the open ocean.

Snow on Antarctic sea ice Reviews of Geophysics, 2001 (Ref: 17058)
Category 1: Peer-reviewed literature

Snow on Antarctic sea ice plays a complex and highly variable role in air-sea-ice interaction processes and the Earth's climate system. Using data collected mostly during the past 10 years, this paper reviews the following topics:

A field trial of in situ chemical oxidation to remediate long-term diesel contaminated Antarctic soil Cold Regions Science and Technology, 2004 (Ref: 11824)
Category 1: Peer-reviewed literature

In situ chemical oxidation (ICO) has been identified as a potential technology for the remediation of petroleum hydrocarbon contaminated sites in Antarctica.

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