Melbourne
17.1 Evaporation from surface water
Supporting information
The volume presented in the water accounting statements (47,133 ML) represents evaporation from the surface of water storages.
The following table presents the breakdown of evaporation from water storages in the Melbourne region during the 2012–13 year.
Storage operator |
Storage |
Volume (ML) |
Melbourne Water |
Cardinia Reservoir |
11,688 |
Greenvale Reservoir |
1,339 |
|
Maroondah Reservoir |
2,126 |
|
O'Shannassy Reservoir |
345 |
|
Silvan Reservoir |
3,351 |
|
Sugarloaf Reservoir |
4,028 |
|
Tarago Reservoir |
3,601 |
|
Upper Yarra Reservoir |
7,799 |
|
Yan Yean Reservoir |
4,820 |
|
Southern Rural Water |
Melton Reservoir |
2,220 |
Merrimu Reservoir |
1,949 |
|
Pykes Creek Reservoir |
1,630 |
|
Rosslynne Reservoir |
2,237 |
|
Total |
47,133 |
Quantification approach
Data source
Provided by
Method
The potential evaporation estimate produced by the Australian Water Resources Assessment system Landscape model (AWRA-L) Version 3.0 (Van Dijk 2010) was used to calculate evaporation from the surface water store. The AWRA-L model uses a modified version of the Penman-Monteith method to produce the potential evaporation. Daily AWRA-L potential evaporation grids were produced based on daily gridded climate data that were available on a 0.05 degree (approximately 5 km) national grid.
Potential evaporation is an estimate of the evaporative demand of the environment. The daily gridded climate datasets used to produce this estimate are generated by the Bureau and include downward solar radiation, and maximum and minimum air temperature. The methods used to generate these gridded datasets are outlined in Jones et al. (2007).
The evaporation at each waterbody was estimated from the proportionally weighted average of grid-point cells that intersected each water feature. The volume was then estimated using the monthly average surface area of each waterbody. The surface area varied dynamically with changing water storage level for reservoirs where the relationship between storage level and surface area had been derived. In the Melbourne region, the surface area of all water storages was calculated dynamically.
Assumptions, limitations, caveats and approximations
- The AWRA-L potential evaporation estimates are subject to approximations associated with interpolating the observation point input data to a national grid as described in Jones et al. (2007)
- The dynamic storage surface areas calculated from the levels and storage rating tables represent a monthly average and therefore will not capture changes that occur on a shorter timescale.
- The total surface area of the surface water store within the Melbourne region included only the water storages not river channels.
- Melbourne Water measures evaporation using the factored pan method. Melbourne Water's calculations of evaporation from water storages during the 2012–13 year were not available for the full reporting period. Melbourne Water evaporation estimates from water storages they managed were shown in the following table:
Storage |
Evaporation volume (ML) |
Evaporation volume (ML) |
|
The Bureau |
Melbourne Water |
Cardinia Reservoir |
12,514 |
* |
Greenvale Reservoir |
1,430 |
1,898 |
Maroondah Reservoir |
2,279 |
1,748 |
O'Shannassy Reservoir |
369 |
257 |
Silvan Reservoir |
3,590 |
* |
Sugarloaf Reservoir |
4,323 |
3,985 |
Tarago Reservoir |
3,847 |
1,756 |
Upper Yarra Reservoir |
8,313 |
5,805 |
Yan Yean Reservoir |
5,147 |
4,685 |
Total |
41,812 |
* |
* 2012–13 evaporation volumes for Cardinia and Silvan reservoirs are unavailable for the full reporting period.