Water resources - Allocation and Use - Western Australia
Western Australia
How has Western Australia's water use changed since 1985?
Comparison between the 1985 and 2000 'snapshot' assessments is difficult. Factors include the time between assessments (more than 15 years); seasonality and variability of climate; significant potential for changes in land use; and fluctuations in domestic and global market demands.
Water Use, Climate and the Audit Baseline Year - 1996/97
The baseline year for the Audit is the 1996/97 agricultural year starting on the 1st April and ending on 31st of March. For water use the data was compiled for the period 1 July 1996 to 30 June 1997 (water calendar year). When it is necessary to collect information for more than one year, the data collected must cover that year or, alternatively, appropriately adjusted to provide a best estimate for that year.
For water use data States and Territories were requested to provide a 5 yearly average value based on the 1996/97 year. Use figures were adjusted in areas where, due to climatic conditions, the water use was not considered to be 'average'.
Climate in 1996/97
During 1996 there was a transition from the weak large-scale climate controls to a strong El Ni?o condition after March 1997. This resulted in a drying over a large part of southern and eastern Australia. From July until September 1996 Victoria had unusually cold and wet weather. The remainder of the southern half of Australia was also wet for three months. Significant areas in south-west Queensland, western and central New South Wales, South Australia, western Victoria, and southern Western Australia had rainfall totals within the highest 10% on record.
During the summer of 1996-97, there was a very active monsoonal season in the tropical zones in western Australia and the Northern Territory. However, this finished abruptly and early, as El Ni?o developed rapidly in autumn 1997. From October 1996 very dry conditions prevailed over most of Victoria, the grain belts of South Australia and north-east Tasmania. Areas of southern Victoria through to south-east South Australia had the driest October to June period on record.
May 1997 brought rain to southern Australia and average to above average rain to parts of Queensland. There was some relief to farmers from the dry and hot conditions over southern Australia in early 1997. In parts of southern Victoria and south-east South Australia the driest October to June period was reported. (ABS Water Account, 2000)
Climate in 1983/84 (Water Review 85)
Water use in any particular year is affected by weather conditions. For much of Australia, the period, July 1983 to June 1984, was equivalent to a normal year in which water use was about average. In south-east Australia, however, abnormal weather patterns were experienced. In general, rainfall totals throughout Victoria were high during the first half of the year but were lower than average in the second half. These weather conditions, along with a continuing sensitivity to water use following the 1982/83 drought, had a marked effect on water usage. Although the 1982/83 drought that affected most of Victoria was broken by above-average rains early in the year, water restrictions in many urban areas were not lifted until much later in the year. Urban water use was therefore less than average, due both to the heavy rains and to the continuance of water restrictions.
The above-average rains in the first half of 1983-84 greatly reduced irrigation demands, and by mid-season virtually unrestricted supplies of water were made available to farmers (for example, 200% of water rights in the Goulburn-Murray Irrigation District). The drier conditions in the latter half of the year somewhat compensated for this, but total usage for the year was generally far less than average.
Rural usage was also less than average, again due to the early wet conditions and sensitivity about excessive water use following the 1982-83 drought. (DPIE, 1987).
Note: The change in water use volume from 1985 to 1996 does not always reflect factors affecting consumption patterns and volumes such as population growth, industry or land-use change or operational improvements. The observed difference may partly be attributed to differences in the approach and assumptions used to estimate water use within the river basin.
| Basin Name | Use in 1983-84 (GL /yr) | Use in 1996-97 (GL /yr) | % Change |
|---|---|---|---|
| WA | 701 | 659 | -6 |
| Albany Coast | 6 | 4 | -34 |
| Ashburton River | 0 | 0 | no data |
| Avon River | 12 | 18 | 52 |
| Blackwood River | 16 | 18 | 16 |
| Busselton Coast | 4 | 7 | 98 |
| Cape Leveque Coast | 1 | 1 | -19 |
| Collie River | 57 | 62 | 9 |
| De Grey River | 0 | 0 | no data |
| Denmark River | 2 | 2 | -45 |
| Donnelly River | 4 | 3 | -23 |
| Drysdale River | 1 | 1 | -53 |
| Esperance Coast | 2 | 1 | -86 |
| Fitzroy River (WA) | 5 | 1 | -84 |
| Fortescue River | 0 | 7 | no data |
| Frankland River | 2 | 2 | -23 |
| Gascoyne River | 0 | 0 | no data |
| Greenough River | 4 | 2 | -49 |
| Harvey River | 73 | 52 | -29 |
| Isdell River | 1 | 1 | -47 |
| Keep River | 1 | 1 | 80 |
| Kent River | 2 | 1 | -53 |
| King Edward River | 1 | 1 | -37 |
| Lennard River | 1 | 1 | -17 |
| Lyndon-Minilya Rivers | 0 | 0 | no data |
| Moore-Hill Rivers | 4 | 4 | -11 |
| Murchison River | 1 | 1 | -33 |
| Murray River (WA) | 15 | 26 | 75 |
| Ninghan | 1 | 1 | 40 |
| Onslow Coast | 0 | 0 | no data |
| Ord River | 48 | 271 | 472 |
| Pentecost River | 1 | 1 | 19 |
| Port Hedland Coast | 0 | 5 | no data |
| Preston River | 4 | 11 | 201 |
| Prince Regent River | 1 | 1 | -36 |
| Shannon River | 10 | 5 | -49 |
| Swan Coast | 4 | 146 | 4,344 |
| Warren River | 10 | 8 | -14 |
| Wooramel River | 0 | 0 | no data |
| Yarra Yarra Lakes | 1 | 1 | -3 |
Note: The total surface water use reported for each river basin does not include the water consumption of the eleven major cities. The data for cities and river basins are reported in the State totals.
How are the surface water resources used and allocated in Western Australia?
Table: Surface water diversion and allocation 1996-97
| Basin/SWMA Name | Allocation (GL/yr) | Diversion (GL/yr) | Diversion: Allocation (%) |
|---|---|---|---|
| Western Australia | 856 | 659 | 0 |
| Albany Coast | 5 | 4 | 77 |
| Avon River | 2 | 2 | 98 |
| Blackwood River | 14 | 14 | 98 |
| Busselton Coast | 7 | 7 | 100 |
| Cape Leveque Coast | 1 | 1 | 100 |
| Collie River | 89 | 60 | 67 |
| Denmark River | 2 | 1 | 78 |
| Donnelly River | 11 | 2 | 16 |
| Drysdale River | 1 | 1 | 100 |
| Esperance Coast | 1 | 1 | 82 |
| Fitzroy River (WA) | 1 | 1 | 100 |
| Fortescue River | 10 | 7 | 63 |
| Frankland River | 2 | 2 | 99 |
| Greenough River | 2 | 2 | 100 |
| Harvey River | 93 | 67 | 72 |
| Isdell River | 1 | 1 | 100 |
| Keep River (WA) | 1 | 1 | 100 |
| Kent River | 1 | 1 | 100 |
| King Edward River | 1 | 1 | 100 |
| Lennard River | 1 | 1 | 100 |
| Moore-Hill Rivers | 4 | 4 | 100 |
| Murchison River | 1 | 1 | 100 |
| Murray River (WA) | 128 | 83 | 64 |
| Ninghan | 1 | 1 | 100 |
| Ord River (WA) | 321 | 271 | 84 |
| Pentecost River | 1 | 1 | 100 |
| Port Hedland Coast | 15 | 5 | 30 |
| Preston River | 4 | 4 | 80 |
| Prince Regent River | 1 | 1 | 100 |
| Salt Lake | 1 | 1 | 100 |
| Shannon River | 5 | 5 | 97 |
| Swan Coast | 115 | 116 | 101 |
| Warren River | 32 | 9 | 28 |
| Yarra Yarra Lakes | 1 | 1 | 100 |
Note: Allocation is not based on 1999-2000 estimates; Diversion based on five-yearly average 1996-97.
Note: In the table above, the total surface water use reported for each river basin does not include the water consumption of the eleven major cities. The data for cities are reported in the State totals. The volume diverted is the total volume of the SWMA's surface water resources diverted for use both within the management area and for export to other management area.
The water use compilations indicate significant growth in water use since the nominal 1983/84 base year of Review85.
In Review85 the estimated gross water consumption in the State, from all sources, was 840 GL/Yr. In this Audit, figures for current use indicate that gross water consumption from all sources, including losses, amounts to 1800 GL/yr. Groundwater use has trebled since Review 85 and surface water use has increased by 40% mostly due to the Ord.
Significant factors, apart from normal economic growth, driving the increased use include mine dewatering (not adequately covered in Review85), significant step-function farm development in the Ord Irrigation Scheme and a widespread increase in self-supplied irrigation activity from surface and underground water sources in the South West Region.
Please note: The tables set out below detailing Level 1 and Level 2 water use categories. The sum of the Level 2 water use volumes will not necessarily equal the total Level 1 water use volumes. This is primarily due to lack of more detailed water use data. However, where Level 2 use = Level 1 use then blank cells in the table does not indicate water use unaccounted for in these categories.
Table: Surface water use in Western Australia 1996-97
| Basin/SWMA Name | Irrigation (GL/yr) | Rural (GL/yr) | Urban / Industrial (GL/yr) | Total (GL/yr) | In-situ (GL/yr) |
|---|---|---|---|---|---|
| Western Australia | 430 | 23 | 207 | 659 | 1,715 |
| Albany Coast | 2 | 2 | 2 | 4 | no data |
| Avon River | 1 | 11 | 7 | 18 | no data |
| Blackwood River | 12 | 3 | 4 | 18 | no data |
| Busselton Coast | 6 | 1 | 1 | 7 | no data |
| Cape Leveque Coast | no data | 1 | no data | 1 | no data |
| Collie River | 60 | 1 | 3 | 62 | no data |
| Denmark River | 1 | 1 | 1 | 2 | no data |
| Donnelly River | 2 | 1 | 1 | 3 | no data |
| Drysdale River | no data | 1 | no data | 1 | no data |
| Esperance Coast | 1 | 1 | 1 | 1 | no data |
| Fitzroy River (WA) | no data | 1 | no data | 1 | no data |
| Fortescue River | no data | no data | 7 | 7 | no data |
| Frankland River | 1 | 1 | 1 | 2 | no data |
| Greenough River | 2 | 1 | 1 | 2 | no data |
| Harvey River | 46 | 1 | 6 | 52 | no data |
| Isdell River | no data | 1 | no data | 1 | no data |
| Keep River (WA) | no data | 1 | no data | 1 | no data |
| Kent River | 1 | 1 | no data | 1 | no data |
| King Edward River | no data | 1 | no data | 1 | no data |
| Lennard River | no data | 1 | no data | 1 | no data |
| Moore-Hill Rivers | 3 | 1 | 1 | 4 | no data |
| Murchison River | no data | 1 | no data | 1 | no data |
| Murray River (WA) | 3 | 1 | 23 | 26 | no data |
| Ninghan | no data | 1 | no data | 1 | no data |
| Ord River (WA) | 263 | 1 | 8 | 271 | no data |
| Pentecost River | no data | 1 | no data | 1 | no data |
| Port Hedland Coast | no data | no data | 5 | 5 | no data |
| Preston River | 11 | 1 | no data | 11 | no data |
| Prince Regent River | no data | 1 | no data | 1 | no data |
| Salt Lake | 1 | 1 | 12 | 12 | no data |
| Shannon River | 5 | 1 | 1 | 5 | no data |
| Swan Coast | 13 | 1 | 134 | 146 | no data |
| Warren River | 8 | 1 | 1 | 8 | no data |
| Yarra Yarra Lakes | no data | 1 | 1 | 1 | no data |
How are Western Australia's groundwater resources used and allocated?
The current total groundwater use in Western Australia is estimated as 1138 GL/yr. By comparison, Review85 estimated a statewide use of 376 GL/yr, although groundwater abstraction data for Review85 may in some cases have been incomplete.
About 25% of current groundwater use is for irrigation (approximately 300 GL/yr) with a dominant proportion (>90%) of that irrigation usage being on the Perth Coastal Plain. Sixty percent of the remaining irrigation use is in the Carnarvon Basin (Gascoyne).
Of the 840 GL/yr used statewide for urban, mining and industrial and over half is used within the Perth Basin, and nearly one third is used in the Yilgarn Division.
The most significant increases in water use since Review85 have occurred in the Perth, Yilgarn and Pilbara Divisions. In the Perth Region a significant increase of abstraction has occurred since Review85 for both urban and irrigation use. The urban, mining, industrial use reflects significant growth in both public water systems and self-supplied use. The irrigation use reflects the vigorously developing, and generally high value, irrigation industry of the Coastal Plain.
Most Groundwater Management Units are in the Category 1 level of utilisation reflecting a generally low level of allocative stress.
Only two of the State's Groundwater Management Units are in Category 4, these being the Murray Cockleshell Gully unit of the Perth Sedimentary Basin and the Collie Sedimentary Basin. Their combined sustainable yield is 11 GL/yr which is small in comparison with the State's estimated total sustainable yield of 6304 GL/yr and both resources are being actively managed with a strategy in place to reduce dependence on groundwater in order to bring extraction within the estimated sustainable limits.
There are a significant number of Category 3 Groundwater Management Units in the Perth region where utilisation is at or near sustainable limits. These include the intensively investigated superficial resources of the Gnangara and Jandakot mounds where environmental water provisions are established at reform standards. They also include the Leederville and Yarragadee confined aquifers which are considered to be fully allocated. Significant work is underway to improve the understanding of these aquifers and their sustainable limits.
In the Goldfields region, large volumes of hypersaline groundwater are extracted for mineral processing and mine de-watering. Extraction rates exceed direct recharge rates and reduction in paleochannel confined aquifer storage volume is accepted as the resource is hypersaline and does not appear to have any detrimental environmental impact. Pressure heads in most paleochannel aquifers appear to stabilise over time due to induced recharge from surrounding areas. Sustainable limits are set to the licensed allocation volumes.
In the Gascoyne region, the Carnarvon alluvial aquifers of the Gascoyne river are considered to be fully allocated. Controlled aquifer storage reductions within safe limits are allowed over the two or three year periods between river flow replenishment events.
The Albany GMU is also considered to be fully allocated.
Amongst these GMUs of high utilisation are a small number where there are issues associated with extractive pressure and a need for appropriate management. An example is in the Carnarvon Basin where a $4M program of capping flowing artesian bores is in progress. In addition, some sub-aquifer areas within these Category 2 or 3 GMUs may be in localised Category 4 situations with other sub-aquifers compensating by their lower allocation levels. Generally, these local situations are managed within the distributive capacity of the aquifer hydraulics.
"GMU"=Groundwater Management Unit "UA"=Unallocated Area
| Province | Use in 1983-84 (GL /yr) | Use in 1996-97 (GL /yr) | % change | Current Alloc (GL/yr) | Current Use : Alloc (%) | GMU / UA |
|---|---|---|---|---|---|---|
| Western Australia | 784 | 1,138 | 46 | no data | no data | GMU |
| no data | no data | UA | ||||
| Albany-Fraser 1 | no data | 1 | 1 | 1 | 100 | GMU |
| no data | no data | UA | ||||
| Albany-Fraser 2 | no data | 0 | 0 | 0 | no data | GMU |
| no data | no data | UA | ||||
| Amadeus | 1 | 15 | 12 | 14 | 85 | GMU |
| 2 | 0 | UA | ||||
| Arunta | 1 | 7 | 4 | 5 | 76 | GMU |
| 3 | 0 | UA | ||||
| Banemall | 0 | 15 | 15 | 15 | 100 | GMU |
| no data | no data | UA | ||||
| Bonaparte | 1 | 3 | 2 | 2 | 100 | GMU |
| 1 | 0 | UA | ||||
| Bremer 1 | no data | 4 | 4 | 4 | 100 | GMU |
| no data | no data | UA | ||||
| Bremer 2 | no data | 5 | 5 | 5 | 100 | GMU |
| no data | no data | UA | ||||
| Calyie-Mcfadden | no data | 0 | 0 | 0 | no data | GMU |
| no data | no data | UA | ||||
| Canning | no data | 17 | 17 | 17 | 100 | GMU |
| no data | no data | UA | ||||
| Capricorn 1 | no data | 0 | 0 | 0 | no data | GMU |
| no data | no data | UA | ||||
| Capricorn 2 | no data | 3 | 3 | 3 | 100 | GMU |
| no data | no data | UA | ||||
| Capricorn 3 | no data | 1 | 1 | 1 | 100 | GMU |
| no data | no data | UA | ||||
| Capricorn 4 | no data | 1 | 1 | 1 | 100 | GMU |
| no data | no data | UA | ||||
| Carnarvon | 1 | 33 | 33 | 33 | 100 | GMU |
| no data | no data | UA | ||||
| Collie | no data | 24 | 24 | 24 | 100 | GMU |
| no data | no data | UA | ||||
| Eucla | 1 | 1 | 0 | 0 | no data | GMU |
| 0 | no data | UA | ||||
| Halls Creek | 1 | 7 | 7 | 7 | 100 | GMU |
| 0 | no data | UA | ||||
| Hamersley | no data | 79 | 79 | 79 | 100 | GMU |
| no data | no data | UA | ||||
| Kimberley | no data | 0 | 0 | 0 | no data | GMU |
| no data | no data | UA | ||||
| Leeuwin | 1 | 3 | 3 | 3 | 100 | GMU |
| no data | no data | UA | ||||
| Marymia | no data | 7 | 7 | 7 | 100 | GMU |
| no data | no data | UA | ||||
| Musgrave | 1 | 1 | 1 | 0 | no data | GMU |
| 1 | 0 | UA | ||||
| Northampton | 1 | 3 | 3 | 3 | 100 | GMU |
| no data | no data | UA | ||||
| Officer | 1 | 1 | 0 | 0 | no data | GMU |
| 0 | no data | UA | ||||
| Ord-Victoria | 1 | 7 | 0 | 0 | no data | GMU |
| 6 | 0 | UA | ||||
| Paterson | no data | 0 | 0 | 0 | no data | GMU |
| no data | no data | UA | ||||
| Perth | 1 | 745 | 745 | 745 | 100 | GMU |
| 1 | 0 | UA | ||||
| Pilbara | no data | 9 | 9 | 9 | 100 | GMU |
| no data | no data | UA | ||||
| Sylvania | 0 | 0 | 0 | 0 | no data | GMU |
| no data | no data | UA | ||||
| Tanami | 0 | 1 | 0 | 0 | no data | GMU |
| 1 | 0 | UA | ||||
| Yilgarn-Gold Fields | 1 | 136 | 136 | 136 | 100 | GMU |
| no data | no data | UA | ||||
| Yilgarn-Murchison | no data | 30 | 30 | 30 | 100 | GMU |
| no data | no data | UA | ||||
| Yilgarn-Southwest | no data | 24 | 24 | 24 | 100 | GMU |
| no data | no data | UA |
Table: Groundwater use in Western Australia 1996-97
| Province | Irrigation (GL/yr) | Rural (GL/yr) | Urban / industry (GL/yr) | In-situ (GL/yr) | Total (GL/yr) | SY (GL/yr) |
|---|---|---|---|---|---|---|
| Western Australia | 281 | 37 | 821 | no data | 1,138 | 6,304 |
| Albany-Fraser 1 | no data | no data | 1 | 1 | 139 | |
| Albany-Fraser 2 | 0 | 0 | 0 | 0 | 65 | |
| Amadeus | 2 | 2 | 12 | 15 | 143 | |
| Arunta | 4 | 3 | 1 | 7 | 159 | |
| Banemall | no data | 1 | 15 | 15 | 66 | |
| Bonaparte | 0 | 1 | 3 | 3 | 1,264 | |
| Bremer 1 | 1 | 0 | 4 | 4 | 34 | |
| Bremer 2 | 1 | 1 | 5 | 5 | 35 | |
| Calyie-Mcfadden | 0 | 0 | 0 | 0 | 95 | |
| Canning | 5 | 2 | 10 | 17 | 827 | |
| Capricorn 1 | 0 | no data | 0 | 0 | 64 | |
| Capricorn 2 | no data | 1 | 3 | 3 | 19 | |
| Capricorn 3 | no data | no data | 1 | 1 | 90 | |
| Capricorn 4 | no data | 1 | 1 | 1 | 64 | |
| Carnarvon | 8 | 16 | 10 | 33 | 245 | |
| Collie | no data | no data | 24 | 24 | 9 | |
| Eucla | 0 | 1 | 0 | 1 | 94 | |
| Halls Creek | no data | no data | 7 | 7 | 219 | |
| Hamersley | no data | 1 | 79 | 79 | 314 | |
| Kimberley | 0 | 0 | 0 | 0 | 84 | |
| Leeuwin | 3 | no data | no data | 3 | 10 | |
| Marymia | no data | 1 | 7 | 7 | 7 | |
| Musgrave | no data | 1 | 1 | 1 | 64 | |
| Northampton | 2 | 1 | 1 | 3 | 17 | |
| Officer | 0 | 1 | 0 | 1 | 183 | |
| Ord-Victoria | 0 | 6 | 2 | 7 | 561 | |
| Paterson | 0 | 0 | 0 | 0 | 20 | |
| Perth | 262 | 14 | 470 | 745 | 1,911 | |
| Pilbara | no data | 1 | 9 | 9 | 159 | |
| Sylvania | 0 | 0 | 0 | 0 | 6 | |
| Tanami | 0 | 1 | 1 | 1 | 153 | |
| Yilgarn-Gold Fields | 1 | 1 | 134 | 136 | 369 | |
| Yilgarn-Murchison | 1 | 1 | 30 | 30 | 107 | |
| Yilgarn-Southwest | 2 | 4 | 19 | 24 | 561 |
Surface and groundwater interactions
There is no data for this state
Further information
- Western Australia Water Resources Assessment 2000 Report
- Western Australia Water Resources Assessment 2000 Technical Report
- Link to data available for download on the:
- Link to the Map Maker to make a map using this information.
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