You may recall when, at the height of summer in 2019, more than a million fish floated to the surface of the Darling River’s Menindee Lakes. Iconic Murray cod and silver perch were among the dead.
A couple of months later, an expert investigation concluded excessive upstream water extractions, compounded by the ongoing drought, were to blame.
In another investigation in 2020, the Murray-Darling Basin Inspector-General reported he was informed that water theft, lack of compliance, unsustainable water extraction rules, and floodplain harvesting were driving the northern basin’s declines in stream flow – the measured volume of water flowing in a river or stream over a given period of time.
And yet, there appears to be a widely held view that we can place most of the blame of drying rivers on climate change. So what’s the truth? And why does it matter?
Our new research investigated the effects of climate change and water resource development on the Darling River over the past 40 years. We found much of the recent decline of river (stream) flow has not been because of climate change, but almost certainly a result of increased water extractions.
This is important, because naming climate change as the primary culprit for drying rivers may let water managers, ministers and irrigation lobbyists off the hook for failing to effectively control water consumption.
Our point isn’t that climate change is not happening – it’s here, it’s now and it’s global in its devastation. But, our research shows climate change shouldn’t be used as a “get out of jail free” card to excuse bad decision-making and poor planning decisions.
What we found
The Baaka-Darling River has nine major headwater dams and tributaries with a total storage capacity in excess of 4,500 billion litres, about equal to nine Sydney harbours. For decades, it has had high rates of water extraction, provided by 15 main channel weirs and more than 1,000 small weirs along its 1,000 kilometre or so length.
Our analyses looked back at 40 years of meteorological trends and water extractions data, then separated the effects of each on declining river flows.
We found between 1981 and 2020, the northern Murray-Darling Basin has become drier (11 millilitres less rainfall per decade, on average) and hotter (by 0.26℃ per decade, on average) – a trend consistent with climate change projections.
These trends reduced stream flows on the nearby, pristine Paroo River by 28%. The Paroo River has had virtually no water extractions in the last 40 years, which means that lower rainfall and higher temperatures completely explain its decline in river flows.
But this is not true for the Baaka-Darling River. We found stream flows declined by 53% at the Baaka-Darling River. Less than half of this decline could be explained by meteorological trends. This means the rest – more than half of the decline in stream flows – was almost certainly due to other factors: namely, increased water extractions.
Further peer-reviewed evidence in support of our conclusion can be drawn from the large, unmetered, and possibly increasing, water extractions associated with floodplain harvesting. This harvesting may be in the order of hundreds of billions of litres per year in the northern Basin, some of which may be illegal.
This is coupled with much smaller increases in metered water extractions along the Baaka-Darling River and its tributaries over the period 2014-15 to 2017-18.
What this means for wildlife
Reduced river flows are profoundly damaging to the ecosystems of the Murray Darling Basin, and its harms accumulate over time. A key pillar of these ecosystems are waterbirds, such as herons, spoonbills, ibis and kingfishers.
Our research investigated the abundance of waterbirds on the Paroo and Baaka-Darling rivers. We found they were more resilient on the Paroo River wetlands than at Menindee Lakes along the Baaka-Darling River.
In 40 years, the average decline in waterbird abundance on the Paroo River Wetlands was 50%, compared to 75% at Menindee Lakes.
We also simulated what would happen if water were to be reallocated from irrigation to increase the flow in the river, during a drought. Our results suggest the resilience of waterbird numbers at Menindee Lakes and nearby could be improved.
Increases in river flows during drought (relative to business as usual) also supports people, as it improves the availability and quality of drinking water in downstream communities, such Wilcannia and Menindee. And it’s crucial for the habitats of fish, wetland plants, trees, mammals, frogs, and reptiles.
Based on our calculations, the annual cost would be around 1.3% of estimated total irrigation profits if 100 gigalitres per year of water were reallocated to increased stream flows. It would be 4% of estimated total irrigation profits if 300 gigalitres per year of water were reallocated to increased stream flows.
Understanding river flows
Understanding why our rivers are getting drier helps us to respond to both the problem of climate changes and to water mismanagement. Fundamental to water management is knowing how much water is in the entire system, where it is, where it goes, and what value it brings. The measurement technologies to answer these questions are available.
If we are to meet the key objects of the Water Act and the Basin Plan, we need to reduce water extractions and to reallocate water on this iconic river to ensure minimum river flows for downstream communities and for critically important environments.
This task is urgent if Australia is to achieve the goal of the Murray-Darling Basin Plan a decade ago: to create and maintain healthy sustainable working rivers.
The last thing Australia needs in a climate change crisis is for water ministers and their advisers to bury their heads in the sand, about what can, and must, be done to ensure a much more sustainable water outcome for all.
Quentin Grafton, Australian Laureate Professor, Crawford School of Public Policy, Australian National University; Gilad Bino, Senior lecturer, UNSW Sydney; John Williams, Adjunct Professor; Long Chu, Associate Professor, Crawford School of Public Policy, Australian National University y Richard Kingsford, Professor, School of Biological, Earth and Environmental Sciences, UNSW Sydney