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The subantarctic region is frequently subject to violent small storms which often arrive with little warning. The most extreme of these are referred to as 'polar lows', and are accompanied by very strong surface winds. They present serious hazards to shipping and are difficult to forecast.
The ocean circulation along the continental margin of Antarctica remains poorly known, primarily due to the lack of long-term measurements of ocean currents over the continental slope.
The overall objective is to characterise the response of Southern Ocean calcareous zooplankton to ocean acidification resulting from anthropogenic CO2 emissions. Simulated increases in anthropogenic CO2 suggest a reduction in the calcification rates of calcareous organisms.
McDonald Island is the southern end of a line of submerged islands (seamounts) evenly spaced, similar to the Hawaiian chain. Here, the earth's crust is stationary so the hypothesis is that the source of lava is moving.
Ozone depletion above Antarctica has caused large increases in springtime UVB radiation (UVBR) and recovery of the ozone layer is not expected until 2060. We have shown that increased UVBR is likely to have more negative effects on the endemic moss, Schistidium antarctici…
This project aims to develop a new method, high resolution capillary electrophoresis - single strand conformation polymorphism (CE-SSCP) for the analysis of ribosomal RNA.
Antarctic fast ice is a crucial climate component, and of critical importance to the survival of higher predators and to shipping and (intra-continental fixed-wing) aircraft operations. Neither its base state nor its variability are well documented.
This project will measure the sea ice thickness off East Antarctica, over spatial scales up to hundreds of kilometers. Sea ice is a likely sensitive indicator of climate variations and change. No large scale sea ice thickness measurements exist in the Antarctic.
This project will assess the importance of the trace micro-nutrient element iron to Antarctic sea-ice algal communities during the International Polar Year (2007-2009).
An ice core drilling expedition is proposed for Aurora Basin, between Law Dome and Dome C. This will provide a climate record in excess of 2000 years and will be used to compare coastal and inland Antarctic records.