The Spirit of Mawson - Australasian Antarctic Expedition 2013 - 2014

Australasian Antarctic Expedition

The Science Case

The Australasian Antarctic Expedition of 1911-1914 resulted in the first complete study of the vast region which lies south of Australia and New Zealand. The three years’ worth of observations gleaned by Mawson and his men provide a unique dataset against which we can compare the changes seen today. Policy documents highlight numerous science questions that need to be urgently addressed across the region. And yet, despite of a century of research, major questions remain about whether the changes seen today are exceptional. The combination of extreme conditions and vast distances involved make the Australasian sector of the Antarctic one of the most problematic to study.

The scale of Antarctica and the Southern Ocean is staggering. Over 98% of the continent is submerged by three large ice sheets that drown the underlying topography. The Australasian sector is dominated by the East Antarctic Ice Sheet, the largest of three ice sheets that contains enough freshwater to raise the world’s sea level by some 52 metres. Until recently it was thought this ice sheet was stable, sitting on the continental crust above today’s sea level. However there is an increasing body of evidence, including by the AAE members, that have identified parts of the East Antarctic which are highly susceptible to melting and collapse from ocean warming.


The surrounding Southern Ocean has an enormous influence on Antarctica, isolating the continent from the rest of the planet. This vast expanse of water is home to the largest ocean current in the world: the Antarctic Circumpolar Current. The size of this current is prodigious, transporting around a million cubic metres of seawater every second. This current plays a crucial role linking the Indian, Atlantic and Pacific oceans, while also acting as one of the great heat and carbon sinks for the atmosphere. Importantly, some 70% of all wind energy going into the world’s oceans enters through the Antarctic Circumpolar Current. Most of the energy comes from the southern hemisphere westerly wind belt – the colourfully named ‘roaring forties’, ‘furious forties’ and ‘screaming sixties’.  Over the last 40 years or so, this wind belt has been shifting south, and as a result caused massive disruption to the circulation of the Southern Ocean and climate of the region. The impacts over the next century are likely to be some of the most significant anywhere on our planet and could have global consequences. The effects of this marked shift in westerly winds are already being seen today, triggering warm and salty water to be drawn up from the deep ocean, melting large sections of the Antarctic ice sheet with unknown consequences for future sea level rise while the ability of the Antarctic Circumpolar Current to soak up heat and carbon from the atmosphere remains deeply uncertain.


Image credit: Ben Maddison

The little explored subantarctic islands in the Southern Ocean have experienced some of the most significant warming. The response of the rich biodiversity in the region to change remains a major area of research, particularly because many of the plants and animals found on and around the islands are subject to numerous pressures. The region is a complex and finely balanced system, with some of the islands still recovering from industrial-scale hunting of whales, seals and penguins. Add climate change into the mixture and the future remains difficult to predict.


A key problem for reducing the uncertainty in climate projections is historical records of change are often too short to test the skill of climate models, raising concerns over our ability to successfully plan for the future. In this regard, the original AAE observations are a crucial dataset, providing an invaluable baseline against which to compare. However, large gaps in our knowledge of past change in the region remain. Fortunately, a wealth of natural archives – such as recorded by trees, peats and lake sediments – provide an opportunity to bridge the gap between modern observations and the recent geological past. Previous work has shown that large-scale shifts have taken place in the past. The causes remain unknown. When and where these tipping points may be reached in the Antarctic continues to be an area of great uncertainty.

The Australasian Antarctic Expedition 2013-2014 is therefore undertaking a programme of research across the region, building on the work 100 years ago, to try to better understand present and future change in Antarctica and Southern Ocean (Figure 1).


Figure 1: The different components of the Australasian Antarctic Expedition 2013-2014 science programme (aligned with the Australian Antarctic Science strategic plan 2011 to 2021).


We are going south to:

  1. gain new insights into the circulation of the Southern Ocean and its impact on the global carbon cycle
  2. explore changes in ocean circulation caused by the growth of extensive fast ice and its impact on life in Commonwealth Bay
  3. use the subantarctic islands as thermometers of climatic change by using trees, peats and lakes to explore the past
  4. investigate the impact of changing climate on the ecology of the subantarctic islands
  5. discover the environmental influence on seabird populations across the Southern Ocean and in Commonwealth Bay
  6. understand changes in seal populations and their feeding patterns in the Southern Ocean and Commonwealth Bay
  7. produce the first underwater surveys of life in the subantarctic islands and Commonwealth Bay
  8. determine the extent to which human activity and pollution has directly impacted on this remote region of Antarctica
  9. provide baseline data to improve the next generation of atmospheric, oceanic and ice sheet models to improve predictions for the future

All our science work has been approved by the New Zealand Department of Conservation, the Tasmanian Parks and Wildlife Service and the Australian Antarctic Division. We are incredibly grateful for all their help and support.

For more information, do feel free to contact us. We hope you can join the team.

Professor Chris Turney and Dr Chris Fogwill
The Australasian Antarctic Expedition 2013-2014
University of New South Wales


Further Reading

Australian Government, 2011. Australian Antarctic Science Strategic Plan 2011–12 to 2020–21. Australian Antarctic Division, Tasmania, p. 74.

Burrows, M.T., Schoeman, D.S., Buckley, L.B., Moore, P., Poloczanska, E.S., Brander, K.M., Brown, C., Bruno, J.F., Duarte, C.M., Halpern, B.S., Holding, J., Kappel, C.V., Kiessling, W., O’Connor, M.I., Pandolfi, J.M., Parmesan, C., Schwing, F.B., Sydeman, W.J. Richardson, A.J., 2011. The pace of shifting climate in marine and terrestrial ecosystems. Science 334, 652-655.

Cook, A.J., Poncet, S., Cooper, A.P.R., Herbert, D.J. Christie, D., 2010. Glacier retreat on South Georgia and implications for the spread of rats. Antarctic Science 22, 255-263.

Fogwill, C.J., Hein, A.S., Bentley, M.J. Sugden, D.E., 2011. Do blue-ice moraines in the Heritage Range show the West Antarctic ice sheet survived the last interglacial? Palaeogeography, Palaeoclimatology, Palaeoecology 335-336, 61-70.

Forcada, J. Trathan, P.N., 2009. Penguin responses to climate change in the Southern Ocean. Global Change Biology 15, 1618-1630.

Gille, S.T., 2008. Decadal-scale temperature trends in the Southern Hemisphere ocean. Journal of Climate 21, 4749-4765.

Kriegler, E., Hall, J.W., Dawson, R. Schellnhuber, H.J., 2009. Imprecise probability assessment of tipping points in the climate system. Proceedings of the National Academy of Sciences 106, 5041-5046.

Le Quéré, C., Raupach, M.R., Canadell, J.G., Marland, G. et al., 2009. Trends in the sources and sinks of carbon dioxide. Nature Geoscience 2, 831-836.

Lenton, T.M., Held, H., Kriegler, E., Hall, J.W., Lucht, W., Rahmstorf, S. Schellnhuber, H.J., 2008. Tipping elements in the Earth’s climate system. Proceedings of the National Academy of Sciences 105, 1786-1793.

Miles, B.W.J., Stokes, C.R., Vieli, A. Cox, N.J., 2013. Rapid, climate-driven changes in outlet glaciers on the Pacific coast of East Antarctica. Nature 500, 563-566.

Pritchard, H.D., Arthern, R.J., Vaughan, D.G. Edwards, L.A., 2009. Extensive dynamic thinning on the margins of the Greenland and Antarctic ice sheets. Nature 461, 971-975.

Sijp, W.P. England, M.H., 2009. Southern Hemisphere westerly wind control over the ocean's thermohaline circulation. Journal of Climate 22, 1277-1286.

Thompson, D.W.J., Solomon, S., Kushner, P.J., England, M.H., Grise, K.M. Karoly, D.J., 2011. Signatures of the Antarctic ozone hole in Southern Hemisphere surface climate change. Nature Geoscience 4, 741-749.

Turney, C., Fogwill, C., Van Ommen, T.D., Moy, A.D., Etheridge, D., Rubino, M., Curran, M.A.J. Rivera, A., 2013. Late Pleistocene and early Holocene change in the Weddell Sea: a new climate record from the Patriot Hills, Ellsworth Mountains, West Antarctica. Journal of Quaternary Science 28, 697-704.

Turney, C.S.M. Jones, R.T., 2010. Does the Agulhas Current amplify global temperatures during super-interglacials? Journal of Quaternary Science 25, 839-843.

Waugh, D.W., Primeau, F., DeVries, T. Holzer, M., 2013. Recent changes in the ventilation of the Southern Oceans. Science 339, 568-570.

Wingham, D.J., Wallis, D.W. Shepherd, A., 2009. Spatial and temporal evolution of Pine Island Glacier thinning, 1995-2006. Geophysical Research Letters 36, doi:10.1029/2009GL039126.

Wunsch, C., 1998. Work done by the wind on the oceanic general circulation. Journal of Physical Oceanography 28, 2332-2340.