Why our rivers are running drier

Publicly released:
Australia; SA
Image of drought impacted Lake Keepit in regional NSW - Image by Wallula from Pixabay
Image of drought impacted Lake Keepit in regional NSW - Image by Wallula from Pixabay

An international team of researchers including the University of Adelaide has demonstrated that climate change is responsible for the changes in the flow and water volume of rivers globally, with major implications for Australia.

Media release

From: The University of Adelaide

An international team of researchers including the University of Adelaide has demonstrated that climate change is responsible for the changes in the flow and water volume of rivers globally, with major implications for Australia.

In the study published in Science, the team investigated changes in river flow, and whether the globally visible changes could be attributed to climate change or to water and land management. The researchers modelled the changes using data collected from 7,250 measuring stations worldwide, including in southern parts of Australia.

While climate change’s impact on water volumes and flooding and drought is widely recognised, this is the first research to examine the changes in river flow globally using direct measurements of stream flow.

The research demonstrated that river flow has changed systemically between 1971 and 2010. Complex patterns were revealed – with some regions including Australia and the Mediterranean becoming drier, while elsewhere such as in Scandinavia, water volumes have increased. The research found that climate change is a key factor in these changes.

Co-author Professor Seth Westra. from the University of Adelaide’s School of Civil, Environmental and Mining Engineering, said: “In Australia, it is increasingly recognised that at least part of the observed decreases in flowing water volumes in our rivers and streams can be attributed to climate change.”

“Historically Australia is known as ‘a land of droughts and flooding rains’ – in that throughout our history there has been times of severe drought but also times where there has been too much water. In the past, those extremes have been largely attributed to natural environmental processes,” Professor Westra said.

“However, because of the drying effect of climate change on our river systems, we can no longer assume history will repeat and we must prioritise mitigating the impact.”

River flow is an important indicator of water resources available to humans and the environment.

“In Australia around 70 per cent of water is used in agriculture production, with much of that water used in the irrigation of crops. Australia’s economy, food security and wellbeing are all dependent on our water resources, so it’s critical we plan for a drier future,” said Professor Westra.

The research acknowledges there are other factors affecting water fluctuations including water management and land use, but found that these were not sufficient to explain global changes. Rather, the global changes in water resource availability could only be understood if climate change was taken into account.

The research was made possible by a collaboration of researchers across 12 countries, and the data collation represents the largest global data set with river flow observations available today. With the models developed from the data, it will be possible to project how rivers will continue to change in the future. Such projections provide an important basis for planning in the affected regions in order to secure water supply and adjust to climate change.

Journal/
conference:
Science
Research:Paper
Organisation/s: The University of Adelaide
Funder: We acknowledge financial support as follows: L.G. and S.I.S. were supported through the H2020 projects CRESCENDO (grant no. 641816) and 4C (grant no. 821003). S.I.S. acknowledges support from the European Research Council through the ERC DROUGHT-HEAT project (grant no. FP7-IDEAS-ERC-617518). H.M.S. is supported in part by the German Federal Ministry of Education and Research (BMBF, grant no. 01LS1711F). H.X.D. is supported by the University of Michigan (grant no. U064474). W.T. acknowledges support from the Uniscientia Foundation and the ETH Zurich Foundation (grant no. Fel-45 15-1). J.L. is supported by the National Natural Science Foundation of China (grant nos. 41625001 and 41571022) and the Strategic Priority Research Program of Chinese Academy of Sciences (grant no. XDA20060402). J.B. acknowledges support from MEXT/JSPS KAKENHI (grant no. 16H06291) and the Environmental Research and Technology Development Fund (grant no. 2RF-1802). Y.P. acknowledges support from the National Science Foundation (grant no. 1752729). Y.S. was supported by the Ministry of Education, Culture, Sports, Science and Technology of Japan (Integrated Research Program for Advancing Climate Models) (grant no. JPMXD0717935715). M.G.G. received support from the Greek State Scholarship Foundation (IKY) (grant no. MIS5033021).
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