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The Responses of Antarctic Sea Ice and Overturning Cells to Meridional Wind Forcing Journal of Climate, 2025 (Ref: 17278)
Category 1: Peer-reviewed literature

Meridional winds over the seasonal ice zone of the Antarctic have undergone changes and likely contributed to sea ice extent variability in recent decades. In this study, using observations and an eddy-resolving channel model of the Antarctic seasonal ice zone…

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…

GPS Radio Occultation for studying the Antarctic Atmosphere and Climate Analysis Strategic Science in Antarctica Conference, Hobart, Australia, 24-26 June 2013, 2013 (Ref: 15552)
Category 3: Poster

This presentation introduces a recently awarded Australian Antarctic Science (AAS) project as part of the research theme 1 'Climate Processes and Change'. This project utilises the technique of Global Positioning System (GPS) Radio Occultation (RO)…

Molecular data can help to unveil biogeographic complexities since the Miocene: lessons from ameronothroid mites and isotomid springtails Online proceedings of the 10th ISAES, USGS Open-File Report 2007-1047, Extended Abstract 008, 2007 (Ref: 13358)
Category 3: Abstract

the glaciation and isolation of the Antarctic continent completed by ~10 million years ago, and not by the sequential break-up of Gondwana (completed by ~32 million years ago). More recently…

Carbon dynamics in an ultra-oligotrophic epishelf lake (Beaver Lake, Antarctica) in summer. Freshwater Biology, 2006 (Ref: 12637)
Category 1: Peer-reviewed literature

1. Microbial plankton dynamics in an ultra-oligotrophic epishelf lake (Beaver Lake, Antarctica) were investigated over an austral summer (December 2002 to January 2003). The aim was to characterise carbon cycling in an environmentally extreme lake. 2.

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