Murray–Darling Basin
17.1 Evaporation from surface water
Supporting information
The volumetric value for the line item at the end of the 2012–13 year was 3,036,866 ML.
The line item represents evaporation volumes from surface water assets within the Murray–Darling Basin (MDB) region. Evaporation from storages (included in line item 1.1); regulated river channels, locks and weirs (included in line item 1.3); lakes (included in line item 1.4); and other known water bodies within the region were taken into account in the line item. Information on evaporation from other surface water assets (mainly unregulated rivers and unknown water bodies) is not available.
Evaporation volumes from surface water assets on water resources plan (WRP) area basis are summarised in the following table. Specific details of evaporation from individual asset basis are included in the table thereafter. In the tables, volumes shown against a WRP or sustainable diversion limit (SDL) area are based on surface water assets geographically located within that area.
Surface WRP area | State/Territory |
Volume (ML) |
|
Code | Name |
||
SW20 | Warrego–Paroo–Nebine | Qld | – |
SW19 | Condamine–Balonne | Qld | 55,935 |
SW18 | Moonie | Qld | – |
SW17 | Qld Border Rivers | Qld | 34,355 |
SW16 | NSW Border Rivers | NSW | 10,867 |
SW12 | Barwon–Darling Watercourse | NSW | – |
SW13 | NSW Intersecting Streams | NSW | – |
SW15 | Gwydir | NSW | 51,442 |
SW14 | Namoi | NSW | 66,883 |
SW11 | Macquarie–Castlereagh | NSW | 92,347 |
Sub-total Northern Basin | 311,829 |
||
SW10 | Lachlan | NSW | 141,038 |
SW9 | Murrumbidgee NSW | NSW | 98,599 |
SW8 | NSW Murray and Lower Darling | NSW | 924,208 |
SW3 | Northern Victoria | Vic. | 287,745 |
SW2 | Vic. Murray | Vic. | 237,951 |
SW4 | Wimmera–Mallee | Vic. | 62,507 |
SW5 and SW7 | SA Murray Region and Eastern Mount Lofty Ranges | SA | – |
SW6 | SA River Murray | SA | 953,358 |
SW1 | ACT | ACT | 19,629 |
Sub-total Southern Basin | 2,725,037 |
||
Total for the region | 3,036,866 |
WRP area | SDLarea |
State/Territory | Surface water asset | Volume (ML) for the 2012–13 year |
|
Code |
Name |
||||
SW19 Condamine–Balonne | SS26 | Condamine–Balonne | Qld | Buckinbah Weir1 | 2,691 |
Chinchilla Weir1 | 4,162 | ||||
Connolly Reservoir2 | 564 | ||||
Cooby Creek Reservoir2 | 3,279 | ||||
Jack Taylor Weir1 | 3,368 | ||||
Lake Kajarabie1 | 28,621 | ||||
Lake Leslie1 | 11,993 | ||||
Moolabah Weir1 | 1,111 | ||||
Neil Turner Weir2 | 147 | ||||
SW17 Qld Border Rivers | SS24 | Qld Border Rivers | Qld | Glenlyon Lake1 | 19,984 |
Lake Coolmunda1 | 13,116 | ||||
Storm King Reservoir2 | 1,255 | ||||
SW16 NSW Border Rivers | SS23 | NSW Border Rivers | NSW | Lake Inverell2 | 481 |
Pindari Lake1 | 10,078 | ||||
Tenterfield Creek Reservoir2 | 308 | ||||
SW15 Gwydir | SS22 | Gwydir | NSW | Lake Copeton1 | 50,315 |
Tareelaroi Weir1 | 1,127 | ||||
SW14 Namoi | SS21 | Namoi | NSW | Chaffey Reservoir1 | 474 |
Dungowen Reservoir2 | 826 | ||||
Gunidgera Weir1 | 720 | ||||
Lake Keepit1 | 39,093 | ||||
Mollee Weir1 | 1,144 | ||||
Quipolly Reservoir2 | 1,293 | ||||
Split Rock Reservoir1 | 23,333 | ||||
SW11 Macquarie–Castlereagh | SS20 | Macquarie–Castlereagh | NSW | Chifley Reservoir2 | 2,964 |
Lake Burrendong1 | 62,728 | ||||
Lake Oberon2 | 4,876 | ||||
Lake Windamere1 | 17,460 | ||||
Rylstone Reservoir2 | 1,024 | ||||
Spring Creek Reservoir2 | 960 | ||||
Suma Park Reservoir2 | 1,781 | ||||
Timor Reservoir2 | 250 | ||||
Winburndale Reservoir2 | 304 | ||||
Sub-total Northern Basin | 311,829 |
||||
SW10 Lachlan | SS16 | Lachlan | NSW | Carcoar Lake1 | 3,554 |
Lake Brewster1 | 67,502 | ||||
Lake Cargelligo1 | 15,335 | ||||
Lake Endeavour2 | 655 | ||||
Lake Rowlands2 | 955 | ||||
Lake Wyangala1 | 53,036 | ||||
SW9 Murrumbidgee NSW | SS15 | Murrumbidgee NSW | NSW | Berembed Weir1 | 1,072 |
Blowering Reservoir1 | 44,858 | ||||
Gogeldrie Weir1 | 2,222 | ||||
Hay Weir1 | 5,078 | ||||
Lake Burrinjuck1 | 39,635 | ||||
Maude Weir1 | 1,975 | ||||
Redbank Weir2 | 194 | ||||
Tombullen Storage1 | 3,565 | ||||
SW8 NSW Murray and Lower Darling | SS18 | Lower Darling | NSW | Lake Cawndilla1 | 142,689 |
Lake Menindee1 | 198,977 | ||||
Lake Victoria1 | 123,772 | ||||
Lake Wetherell1 | 90,185 | ||||
Pamamaroo Lake1 | 86,588 | ||||
Stephens Creek Reservoir2 | 8,892 | ||||
SS14 | NSW Murray | NSW | Lake Hume1 | 164,220 | |
Upstream of Lock 7 (Rufus)2 | 5,277 | ||||
Upstream of Lock 8 (Wangumma)2 | 7,657 | ||||
Upstream of Lock 9 (Kulnine)2 | 12,241 | ||||
Upstream of Lock 10 (Wentworth)2 | 11,417 | ||||
Upstream of Lock 15 (Euston)2 | 72,295 | ||||
SW2 Vic. Murray | SS3 | Kiewa | Vic. | Lake Guy2 | 116 |
Rocky Valley Storage2 | 2,036 | ||||
SW3 Northern Victoria | SS4 | Ovens | Vic. | Lake Buffalo1 | 3,870 |
Lake William Hovell1 | 1,603 | ||||
SS5 | Broken | Vic. | Lake Nillahcootie1 | 5,374 | |
McCall Say Reservoir1 | 313 | ||||
SS6 | Goulburn | Vic. | Goulburn Weir 1 | 10,640 | |
Greens Lake1 | 6,167 | ||||
Lake Eildon1 | 126,354 | ||||
Waranga Basin1 | 44,830 | ||||
SS7 | Campaspe | Vic. | Campaspe Weir2 | 241 | |
Lake Eppalock1 | 27,942 | ||||
Lauriston Reservoir2 | 2,163 | ||||
Malmsbury Reservoir2 | 2,994 | ||||
Upper Coliban Reservoir2 | 2,903 | ||||
SS8 | Loddon | Vic. | Barkers Creek Reservoir2 | 514 | |
Cairn Curran Reservoir1 | 15,615 | ||||
Crusoe Reservoir2 | 295 | ||||
Evansford Reservoir2 | 253 | ||||
Hepburn Lagoon2 | 910 | ||||
Kow Swamp2 | 23,334 | ||||
Laanecoorie Reservoir 1 | 3,667 | ||||
McCay Reservoir2 | 200 | ||||
Newlyn Reservoir 1 | 594 | ||||
Sandhurst Reservoir2 | 296 | ||||
Spring Gully Reservoir2 | 373 | ||||
Tullaroop Reservoir1 | 6,300 | ||||
SW2 Vic. Murray | SS2 | Vic. Murray | Vic. | Kangaroo/Racecourse Lake2 | 11,772 |
Lake Banimboola2 | 726 | ||||
Lake Dartmouth1 | 76,447 | ||||
Lake Mulwala1 | 42,368 | ||||
Mildura Weir2 | 1,341 | ||||
Reedy/Middle Lake2 | 3,927 | ||||
Third Lake2 | 2,260 | ||||
Torrumbarry Weir1 | 11,097 | ||||
Upstream of Lake Mulwala2 | 42,368 | ||||
Upstream of Mildura Weir2 | 43,492 | ||||
SW4 Wimmera–Mallee | SS9 | Wimmera–Mallee | Vic. | Dock Lake1 | 5,158 |
Green Lake1 | 6,191 | ||||
Lake Batyo Catyo1 | 505 | ||||
Lake Bellfield1 | 5,624 | ||||
Lake Fyans1 | 4,182 | ||||
Lake Lonsdale1 | 13,669 | ||||
Lake Taylor1 | 3,342 | ||||
Lake Whitton2 | 749 | ||||
Pine Lake1 | 3,477 | ||||
Toolondo Reservoir1 | 8,709 | ||||
Wartook Reservoir1 | 10,900 | ||||
SW6 SA River Murray | SS11 | SA Murray | SA | Blanchetown Weir – Lock 11 | 40,832 |
Bookpurnong Weir – Lock 41 | 7,590 | ||||
Lake Albert1 | 169,942 |
||||
Lake Alexandrina1 | 640,479 |
||||
Overland Weir – Lock 31 | 13,162 | ||||
Renmark Weir – Lock 51 | 8,984 | ||||
Upstream of Lock 6 (Murtho)2 | 14,004 | ||||
Upstream of Lake Alexandrina2 | 46,280 | ||||
Waikerie Weir – Lock 21 | 12,085 | ||||
SW1 ACT | SS1 | ACT | ACT | Bendora Reservoir1 | 924 |
Corin Reservoir1 | 3,098 | ||||
Cotter Reservoir1 | 474 | ||||
Googong Reservoir1 | 7,687 | ||||
Lake Burley Griffin 2 | 5,707 |
||||
Lake Ginninderra2 | 1,012 |
||||
Lake Tuggeranong2 | 728 |
||||
Sub-total Southern Basin | 2,725,037 |
||||
Total for the MDB region | 3,036,866 |
1 Dynamic surface area was used in calculations
2 Static surface area used (based on boundaries defined for surface water bodies in Bureau of Meteorology's Australian hydrological geospatial fabric (AHGF)
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 0.050 (approximately 5 km) national grid.
Potential evaporation was an estimate of the evaporative demand of the environment. The daily gridded climate data sets used to produce this estimate were generated by the Bureau and included downward solar irradiance, and maximum and minimum air temperature. The methods used to generate these gridded data-sets have been outlined in Jones et al. (2007).
The evaporation at each waterbody was estimated from the proportionally weighted average of grid-pixels 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 level for storages where the relationship between storage level and surface area had been derived, where this relationship was not available the static AHGF surface area was used.
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 do not capture changes that occur on a shorter time-scale.
- The use of the static default AHGF surface area is an approximation only. It represents the waterbody at capacity and therefore likely results in an overestimation of precipitation on those features.
Uncertainty information
Comparative year
There was a prior period error in the line item volume reported in the 2012 Account. The prior period error was a result of using solar radiation data with bias correction errors. Solar radiation is an input for line item volume calculation. The line item volume for the 2011–12 year has been recalculated accommodating the prior period error correction. The changes and their respective values are detailed in the following table.
Segment | 2013 Account volume for the 2011–12 year (ML) |
2012 Account volume for the 2011–12 year (ML) |
Difference due to a prior period error (ML) |
Northern Basin | 313,670 | 366,255 | (52,585) |
Southern Basin | 2,672,732 | 2,892,164 | (219,432) |
Whole region | 2,986,402 | 3,258,419 | (272,017) |