River

Flow

A look at the flow and management at key locations

There is an uncontrolled inflow from high flows on the Darling River and a controlled inflow from Lake Cawndilla that feeds into the Darling Anabranch at Redbank Creek. This makes for one of the more complicated systems to track the flow down.

As a general rule, most high flow events in the lower Darling are caused by winter rainfall in central and northeastern NSW that arrive in late winter and spring, while it is the summer monsoon rainfall in southern Queensland that arrive in autumn.

Some key observations of some recent flow events are noted below:

Quick Summary

The Great Darling Anabranch at the offtake needs around 500 ML/day for pleasant paddling, which is around 14,000 ML/day on the Darling. This is just below a minor flood level.

Cawndilla Channel feeds into the lower Tandou Creek and usually has a small envirnmental flow, albeit not nessarily paddable. A flow of around 1,000 ML/day as measured in the Lake Cawndilla Outlet should provide an enjoyable journey if there is water downstream of at least 250 ML/day.

The speed of the flow through the system is fairly slow, just 8 km/day, so a longer prolonged flow is best.

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History

From 1890 to 1961 water flowed the full length of the Darling Anabranch to the River Murray just nine times.

From 1962 to 2008, there was an annual regulated release into the system that is no longer applicable with the new water pipeline for landowners along the system.

Since 2007 up until 2023, the upper anabranch has only flown naturally five times; in Jan 2010, Mar 2011, Mar 2012, Feb 2022 and a ten month long flow event between May 2022 and Feb 2023. Releases from Lake Cawndilla in 2013 and 2017 provided the other two flow events along the lower anabranch.

Mar 2011 and 2012 saw a high flow from both the Lakes and the Darling. The resulting flow pattern was irregular until the high flows that were seen a number of months after the water release started. Flow of approx. 1,000 ML/day were seen in the lower anabranch for around 6 months.

Late 2013 was from Lake Cawndilla at around 1,000 ML/day. This was seen downstream but with a significantly smaller flow with a reduced flow window that would have been hard to paddle.

Autumn 2017 saw a controlled release from Lake Cawndilla, no flow from the Darling River. This provided a clean flush down the entire anabranch and would have been a comfitable paddle.

Summer 2017-18 saw a slightly smaller release from Lake Cawndilla of around 700 ML/day. Most of the water did not reach the lower anabranch and was likely utilised for irragation or simply lost in the heat of summer.

Mid-2021 to 2024 saw a small controlled release from the lakes, followed by a high flow from the Darling. This provided nearly two years worth of good flow to the lower anabranch, including some widespread flooding at the peak that filled most of the lakes other than Lake Tandou.

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Anabranch Start to Flow

Darling Anabranch Offtake rarely flows. The Darling needs to be above the 6 m mark before water naturally splits over the banks.

The following two images show a rising Darling river and the start of the flow into the Darling Anabranch at around the 6 m mark.

graphs
graphs

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Lakes

To complicate matters, there is a series of 16 lakes along the Darling Anabranch that range from 120 to 11,000 ha in size. Water can be diverted into the lakes making it difficult to forecast the flow along the system. For example, in 2022, the high flows from both the Lakes and the Darling itself were mainly being diverted into the lakes. An uncontrolled flow into Popio Lake was still taking approximately two thirds of the remaining flow from the system as I paddled past. This is more likely to occur after the initial peak flows down the system as they try to minimise the impacts of prolonged flooding to the river banks. You should be able to see the lakes fill from the National Maps DEA Surface Reflectance (Sentinel-2 Near Real-Time). This will give you some idea of what is happening in the middle section of the anabranch before the gauge at Dam 183.

A similar thing happened on my second trip, with the lake inflows significantly buffering the flow down the system.

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Flow Speeds

While smaller than the other flows, the 2017 event seems to be the best indicator of the time it takes for water to flow through the system. It appears to be rather slow at around 8 km per day so don't expect much paddling assistance and nearly two months if you are following a flow peak.

With that in mind, you will likely want to see a good flow event to push water down the system for a number of weeks before starting out, along with a consistent flow at both Wycot and Dam 183 (Old Broken Hill Crossing) to ensure water is not being lost into the lower lakes.

Gauge Distances (from Murray)

516 km
Lake Cawndilla
468 km
Packers Crossing
443 km
Offtake
394 km
Wycot (+49–74 km)
212 km
Dam 183
124 km
Bulpunga
73 km
Tara Down
0 km
Murray River
Location Mid* Main* Peak KM Days Speed
L. Cawndilla 19 Feb 01 Mar 1,300
Packers Xing 26 Feb 05 Mar 1,150 48 7 6.8
Wycot 07 Mar 14 Mar 1,000 74 10 7.4
Dam 183 03 Apr 13 Apr 915 182 28 6.5
Bulpunga 14 Apr 20 Apr 875 88 11 8.0
Tara Downs 22 Apr 27 Apr 850 51 8 6.4

*Approx arrivial dates of the mid and main flows.
Peak flow is measured in MLD, and speed in KM per day.

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Personal Experience

I paddled Cawndilla Channel, Tandou Creek, Redbank Creek and the upper section of the Anabranch on around 1,000 ML/day. This provided great paddling conditions, but there were a few spots where a lower flow could become problematic, namely upper Tandou Creek, and the snaggy and tree-filled sections of the other areas. It is difficult to estimate the point where paddling around the thickets of trees will become unnavigable. Similar thickets on the lower anabranch were navigated with a lower flow.

Due to an uncontrolled redirection of water into Popio Lake, I mostly paddled the lower section at 300 ML/day. The conditions with this flow were generally easier than in the top section due to cleaner pools and channels. At this height I ran three channelled flowing sections and a number of wider flowing or pool sections that were shallow, but I only grounded the kayak a small number of times. I wouldn't be alarmed to paddle here in a slightly lower flow but due to the groundings I would recommend a slightly higher flow, somewhere between 400 ML/day and 500 ML/day.

My second trip down was on a much higher flow, and I paddled both Tandou and Coonalhugga creek when the Darling was in minor flood, before the major floods of summer 2022/23.

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Tandou and Coonalhugga Creeks

The other two ways into the anabranch are a bit more complex and only flow when the lower Darling is in flood.

satellite imagery

The upper Tandou Creek appears to start flowing at 18,000 ML/day but not nessarily into the anabranch initially due to a blockbank beside Cawndilla Channel forcing water north into two wetlands. The wetlands started back filling on 2022-01-13 with a flow of 18 GL/day at Main Weir and these took a fortnight to fill. There was minimal evidence of light green waters from Lake Cawndilla mixing with the flood waters downstream of the blockbank. A short portage would be required unless the blockbank gets removed.
Key:
A: Cawndilla Channel
B: Wetlands
C: Blockbank Tandou Creek

I paddled this with a flow of 21.1 GL/day at Weir 32 that provided a nice flow for the top section, although I wouldn't want it to be too much lower. The "real" downstream entrance was not following at this height.

satellite imagery

Coonalhugga Creek started to flow around 2022-07-17, or about 19 GL/day on the Darling. The creek was fully flooded in Dec at 22 GL/day.

Note that some lakes and the floodplains will cannibalise much of the early flow, like Bintullia Lake fills before much flow makes it across Old Pooncarie Rd.
Key:
A: Coonalhugga Creek
B: Bintullia Lake
C: Old Pooncarie Rd

I paddled this at 21.2 GL/day with what seemed to be about the minimum amount of flow. Old Pooncarie Rd started flooding three weeks earlier at 18.5 GL/day, suggesting it takes a while to flush if dry.