Average rainfall during winter 2017 contributed to high natural flows in the Glenelg catchment. The high flows met many of the environmental flow objectives for winter and spring, and it eliminated the need for managed environmental flow releases. Passing flows were also suspended at various times during winter and spring to reduce the flood risk to communities downstream of Rocklands Reservoir. Water accumulated as a result of the suspended passing flows was used to help meet environmental objectives in summer.
The high natural flows during winter/spring and the provision of water for the environment during the summer/ autumn period maintained connectivity from Rocklands Reservoir to the estuary at Nelson throughout 2017–18. Seasonal fluctuations in flows and water levels throughout the year provided opportunities for aquatic plants and animals to disperse between river reaches and to also access a variety of habitats throughout the system. The flows also supported the health of riparian vegetation and the transfer of nutrients and debris from the riverbanks into the river channel. Continuous low flows maintained the quality and quantity of water in riffle-pool habitats. Occasional freshes reduced salinity and water temperature and increased dissolved oxygen concentrations in deeper pools along the river system.
The natural and managed flows in the Glenelg River during 2017–18 provided habitat for native fish and opportunities for fish dispersal, migration and spawning. Young-of-year tupong and estuary perch were recorded more than 40 km upstream of the estuary in summer 2017–18. Strong
migration of these fish species from the estuary corresponds with managed releases of water for the environment, which trigger migration and facilitate movement across habitats that are impassable at lower flows.
Allocations to the environment reached 81 percent in September 2017, based on water reserves from the wet 2016–17 season and good inflows into storages during early winter 2017. Conditions turned to dry during spring, with below-average rainfall and no inflow to storages between November 2017 and April 2018. As a result, there were no additional allocations to the environment after September 2017. Accumulated passing flows were used to meet environmental demands between late spring and mid-January 2018. Water allocated to the environmental entitlement was used to meet demand after that.
In November 2017, the first-ever release of water for the environment was delivered to reach 0 from Moora Moora Reservoir. The release aimed to improve understanding of water movement in the reach and how water can be delivered from the reservoir. Temporary gauges installed in reach 0 showed a significant rise of the river level following the release, but due to a significant rainfall event the full extent of the flow could not be measured accurately. Despite the measurement uncertainty, the trial release improved understanding of the potential for releases of water for the environment to support the important environmental values in reach 0 in the future.