Murray–Darling Basin
1.4 Lakes and wetlands

Supporting information

The volumetric value for the line item for the 2012–13 year was 1,799,526 ML.

This line item represents the volume of water held in lakes and wetlands that are connected either seasonally or perennially to the river channel system. Specific details of individual lakes and wetlands are provided in the following table. Information is provided only for selected lakes and wetlands in the Southern Basin of the Murray–Darling Basin (MDB) region. For other lakes and wetlands, particularly in the Northern Basin, the volumetric values were not available.

Water from lakes and wetlands listed for the line item is not used primarily to supply water for licensed entitlements. Line item 1.1 Storages includes storages that are used to supply water for licensed entitlements.

Details of lakes and wetlands in the MDB region at the start and end of the 2012–13 year
Water resource plan area

Sustainable diversion limit area


Lake name

Total capacity1 (ML)

Total storage2 volume at 30 June 2013 (ML)

Total storage3 volume at 30 June 2012 (ML)



SW4 Wimmera–Mallee SS9 Wimmera–Mallee Vic. Dock Lake  4,430 0 0
Vic. Green Lake  5,350 2,750 3,591
Vic. Lake Batyo Catyo 2,250 9 479
Vic. Pine Lake  62,380 4,019 7,830
SW6 SA River Murray SS11 SA Murray SA Lake Albert 279,583 248,675 250,889
SA Lake Alexandrina 1,644,884 1,509,442 1,513,961
SW1 ACT SS1 ACT ACT Lake Burley Griffin 33,723 29,131 29,122
ACT Lake Ginninderra 3,700 3,700 3,700
ACT Lake Tuggeranong 1,800 1,800 1,800
Southern Basin  2,038,100 1,799,526 1,811,372
Whole MDB region 2,038,100 1,799,526 1,811,372
1–3 Dead storage volumes are included except for Dock Lake, Lake Batyo Catyo, Green Lake, and Pine Lake.

Lakes Burley Griffin, Ginninderra and Tuggeranong are used primarily for recreation, conservation, and aesthetic purposes, and are not formally associated with the urban water supply system; however, water from these lakes can be abstracted or released to maintain environmental flows and for small-scale irrigation.

At present, abstraction from Lake Ginninderra and Lake Tuggeranong is limited to volumes that would have negligible effect on the volume of the lakes (less than 50 ML).

Quantification approach

Data source

(1) Environment and Sustainable Development Directorate of the ACT Government: Lakes Ginninderra and Tuggeranong; (2) National Capital Authority: Lake Burley Griffin; and (3) Bureau of Meteorology (the Bureau)'s Water Storages, Australian Water Resources Information System (AWRIS): other lakes.


Provided by

Environment and Sustainable Development Directorate of the ACT Government, National Capital Authority and the Bureau.



Lakes Ginninderra and Tuggeranong

No storage volume or level information was available for these lakes; however, their capacity is known. Therefore, the total storage within these lakes was estimated based on the assumption that these water bodies were full at the start and end of the year.

Lake Burley Griffin

The volume was as estimated by National Capital Authority.

Other lakes

Storage volume was estimated at the start and end of the year by using gauged water level height(s) (metres Australian height datum) for individual storages. The height measurement was converted to a volume using the storage-volume curve(s) of the storage.

Assumptions, limitations, caveats and approximations

Lakes Ginninderra and Tuggeranong

Water levels in Lake Ginninderra and Lake Tuggeranong are generally managed within 200 mm of full supply level throughout the year. Therefore, the estimated storage volumes of these lakes in the water account are considered to be only slightly overestimated.

Lake Burley Griffin

The capacity of Lake Burley Griffin is based on survey data collected at the time of construction and fill in 1964.

Other lakes

Storage-volume curves represent specifically surveyed parts of the water storage and may not reflect the storage-volume relationship across the entire storage.

Water storages are subject to sedimentation and other physical changes over time, which in turn affect the accuracy of the storage-volume curves.

Uncertainty information

The uncertainty estimate was not quantified.