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Published: 2009

Climate change, not drought, the main suspect


In another CAWCR study, researchers have concluded that the 1996–2009 drought can be attributed to climate change, not natural variability.1

Dry lagoon on the Murray – decreased rainfall since 1993 in south-eastern Australia has been more strongly linked to climate change.
Dry lagoon on the Murray – decreased rainfall since 1993 in south-eastern Australia has been more strongly linked to climate change.
Credit: ScienceImage/Greg Rinder

The Bureau’s Dr Bertrand Timbal said rainfall in south-east Australia has decreased over the past 13 years because the subtropical ridge – a band of high-pressure systems over the south of the continent – has become bigger, stronger and more frequent.

Dr Timbal found that 1996–2009 was the driest period in the 110 years of the Bureau’s records for south-east Australia, surpassing the previous driest period during WWII, and with the most significant annual rainfall declines occurring in autumn and spring.

He pointed out that this seasonal rainfall change ‘now more closely resembles the picture provided by climate model simulations of future changes due to enhanced greenhouse gases’.

When the CAWCR scientists ran computer simulations to establish ‘natural’ influences on temperature, such as changing levels of solar activity, they found no intensification of the subtropical ridge and no decline in rainfall.

But when they added increased greenhouse gas emissions, aerosols and ozone depletion, their modelling results showed strengthening of high-pressure systems in south-east Australia, causing up to 80 per cent of the drop in rainfall across the region.

A recent US study 2 assessed, for the first time, the combined impact on global temperature of four factors: human influences such as carbon dioxide and aerosol emissions; heating from the sun; volcanic activity; and the El Niño southern oscillation.

The analysis shows the relative stability in global temperatures in the last seven years is explained primarily by the decline in incoming sunlight associated with the downward phase of the 11-year solar cycle, together with a lack of strong El Niño events. These trends have masked the warming caused by carbon dioxide and other greenhouse gases.


1 Timbal B (2009) The continuing decline in south-east Australian rainfall: update to May 2009. In: CAWCR Research Letters 2, July 2009. (Eds PA Sandery, T Leeuwenburg, G Wang and AJ Hollis.)
2 Lean JL and Rind DH (2009) How will Earth’s surface temperature change in future decades? Geophysical Research Letters 36, L15708, doi:10.1029/2009GL038932.





Published: 2009

Northern water assessment informs development capacity

Helen Beringen

It either doesn’t rain or it pours up north. Such variability is one of the challenges identified in the first consistent, analytical water assessment of northern Australia released from CSIRO’s Water for a Healthy Country Flagship. The work is informing thinking about the development capacity of the region.

Regional coverage of the Northern Australia Sustainable Yields Project.
Regional coverage of the Northern Australia Sustainable Yields Project.
Credit: CSIRO

Rainfall and runoff variability are just two components of a comprehensive review of water resources for water policy decisions which form part of the assessments undertaken by the Northern Australia Sustainable Yields Project.

Released by Parliamentary Secretary for Water, Dr Mike Kelly, at the RiverSymposium in Brisbane on 21 September, the study resulted from a March 2008 agreement by Council of Australian Governments (COAG) to extend the CSIRO work on sustainable water yields and availability that had been completed in the catchments of the Murray-Darling Basin.

Dr Kelly said the research would be a valuable resource to inform decisions about the conservation and development of northern Australia’s water resources.

‘From Broome in Western Australia to Cairns in Queensland, the Northern Australia Sustainable Yields (NASY) reports provide important information on current and likely future water availability in northern Australia,’ he said.

Despite popular perceptions that northern Australia has a surplus of water, the research found the extremely seasonal climate with continuously high temperatures meant that the landscape was annually water-limited, with little or no rain for three to six months every year, and very high potential evapotranspiration rates.

‘Northern Australia experiences high rainfall during the wet season, with most falling near the coast and with year to year amounts that are highly variable,’ said project leader Dr Richard Cresswell.

‘Runoff follows a similar pattern to rainfall, with most surface flow approaching the estuaries, with potential inland dam sites receiving less and quite variable amounts of water and suffering very high evaporation rates.

‘The very few river reaches that flow year-round are mostly sustained by localised groundwater discharge and have high cultural, social, ecological and developmental value,’ he said.

‘Groundwater may offer potential for increased extractions for development, though the highly dynamic nature of shallow aquifers, which rapidly fill during the wet season and drain through the dry season, means there is little opportunity to increase this groundwater storage and careful management is required where these groundwaters also provide sources for the few perennial rivers.’

Dr Cresswell said future climate predictions for the north suggest that evapotranspiration was likely to increase while rainfall was likely to be similar to historical levels, which were lower than the last decade, particularly in the west.

Speaking to ABC Rural, Joe Ross, Chair of the federal government’s Northern Australia Land and Water Taskforce (charged with finding new development opportunities in Northern Australia), said the CSIRO report confirmed that expectations for food production in the north have been ‘over the top’, and that there would be limited opportunity for broad-scale agriculture in the tropics.

The Taskforce’s submission to the government later this year will take into account the central findings of the CSIRO teams’ work. ‘It covers not only the amounts of water in northern Australia, but also what impact there’ll be on the livelihoods of the community of northern Australia, in particular, one of the main constituents being Indigenous Australians,’ Mr Ross said.

The Northern Australia Sustainable Yields Project is part of the Australian Government’s Northern Australia Water Futures Assessment (NAWFA), a five-year program to develop an enduring knowledge base to inform decisions about conservation and development of northern Australia’s water resources, so that any development proceeds in an ecologically, culturally and economically sustainable manner.


More information:

Dr Richard Cresswell: Richard.cresswell@csiro.au







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