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The Earth beneath Antarctica is not cold and static but highly dynamic. Its changing shape results from past and present changes in the amount of ice resting on it as well as forces internal to the Earth. These are very poorly understood in Antarctica, and in East Antarctica in particular.
Paradoxically, climate warming increases plant injury and death from freezing and heat-induced water stress. Survival depends on a functional water transport system.
This airborne geophysics and oceanography project explores the Antarctic ice sheet structure, bedrock and changing ice volume to answer key questions about Antarctica and it's contribution to and current and future sea-level rise.
This project aims to characterise the UVR environment in Antarctica and Macquarie Island by continuously monitoring the UV Index at each of the Australian Antarctic research stations.
Geoscience Australia operates an integrated geodetic and geophysical observing system in Australia, its neighbouring region and Antarctica. This science program represents the Antarctic and sub-Antarctic components of this system. It consists of four key elements:
Long-term continuous data sets are critical for monitoring and understanding the Antarctic environment and its interactions with the Earth-system.
Antarctic krill are a fundamental component of Southern Ocean ecosystems and perturbations to krill populations have ramifications for the entire ecosystem. Krill are fished across the Southern Ocean and sustainable management of this fishery is a high priority for the Australian Government.
Australia is a leader in east Antarctica, yet we have only a very limited understanding of the biodiversity of terrestrial, lake and coastal ecosystems of this area.
The aim of the Million Year Ice Core Project (MYIC) is to drill and recover an ice core that extends to well over a million years ago.
The Australian Antarctic Territory has contributed as much as one quarter of the total recent Antarctic ice-mass loss. Here, the Denman Glacier, which holds a potential sea level rise of 1.5 m, is one of the fastest retreating glaciers. However, the causes behind these changes remain a mystery.