Latest updates
Gravity waves are atmospheric waves that play a critical role in defining the dynamical state of our atmosphere.
Located ~1500 km southeast of Tasmania, Macquarie Island is the only place on Earth where oceanic crust and mantle are preserved and undeformed above sea level.
Global sea level fluctuations are driven by changes in the mass balance of the world's ice sheets and mountain glaciers. These fluctuations arise from either the increased discharge of ice into the oceans or through increases in snowfall over these ice masses.
The project has the potential to transform understanding of the physical processes governing drift of the Antarctic ice edge.
Concentrations of aerosols in the polar front atmosphere above the Antarctic sea-ice differ significantly from those in the adjacent regions of the Antarctic continent and the Southern Ocean.
We propose to investigate changes in Southern Hemisphere (SH) hydroxyl radical concentration ([OH]) over the industrial period.
Melting of grounded ice mass in the Arctic and Antarctic may play a key role in future global sea level rise and Earth's climate system. The Antarctic Ice Sheet is losing ice at an increasing rate, primarily due to ocean-driven melting beneath ice shelves.
Understanding how, where and why ice sheets lose mass is an international scientific priority to meet the challenges of global change. The Totten Glacier is a major outlet glacier draining a large area of East Antarctica.
Sea ice plays a key role in Southern Ocean physics and biogeochemical cycles, and is a major driver of Antarctic marine ecosystem processes. In terms of supporting marine food webs, sea ice provides a substrate for ice algae which serve as food source for pelagic herbivores.
The aim of this project is to challenge our global understanding of carbon fixation. In most ecosystems, phototrophic carbon fixation by plants, algae and cyanobacteria is the primary production strategy supporting higher trophic life.