Track water storage, capacity and historical trends for major reservoirs in New South Wales, Victoria, Queensland and beyond.
The storage situation at Lake William Hovell remains highly stable. At 89.4% capacity, the facility is holding 14 GL of water. This volume provides a solid foundation for both urban and agricultural demands across Victoria.
The King River acts as the primary lifeblood for Lake William Hovell, making it a cornerstone of the Murray-Darling Basin network. Hydrological health in this specific drainage basin is vital for downstream ecosystems. Catchment dynamics in the Murray-Darling Basin are deeply influenced by the retention capacity of Lake William Hovell.
Agriculture in the surrounding areas of Victoria depends heavily on the water security provided by Lake William Hovell. Irrigation allocations are directly tied to these storage metrics. Without the buffer provided by this massive 14 GL storage, regional farming would face extreme volatility.
The surrounding catchment of Lake William Hovell also supports diverse local flora and fauna. During periods of healthy water levels, the area often sees an increase in recreational activities such as fishing, boating, and camping. However, environmental flow releases must be carefully balanced to protect downstream river health.
With a mild reading of 6°C today, surface evaporation is significantly reduced, helping to preserve current volume. Recent rainfall measuring 0.1mm in the immediate vicinity is actively contributing to the reservoir's recharge.
The Bureau of Meteorology's climate outlooks will play a pivotal role in predicting the future inflows for this catchment. Continuous telemetry and advanced hydrological modeling are employed to forecast storage changes. Resilience against extreme weather events remains the ultimate goal for the managers of this critical infrastructure.