Summary of the total water resources in the basin
The total volumes of water available and supplied from water resources in the Roper River are shown in Table 2.
In 2004-05 there was no formal environmental water reserve established in the Roper River WMA. The 80:20 Rule was in effect (80% for the environment and 20% for consumption) via the Roper River management plan. In 2004-05 the environment’s share of total flow within the Roper River was 5,540,000 ML (i.e. approximately 99% of total inflows).
Table 2 Summary of water balance in the Roper River water management area, 2004‑05
| Captured Rainfall (or total available water, or rainfall for storage) |
3820214
(runoff) |
1730668
(recharge) |
5550882 |
| Evapotranspiration |
10049 |
0 |
10049 |
| Returns from the economy (includes treated effluent) |
0 |
0 |
0 |
| Extraction & Diversions |
526 |
307 |
833 |
| Losses |
0 |
0 |
0 |
| GW/SW Interaction Volume |
1708904 |
0 |
0 |
| Transfers In |
0 |
0 |
0 |
| Transfers Out |
0 |
0 |
0 |
|
Inflows from other entities |
0 |
0 |
0 |
| Outflows to other entities |
5540000 |
0 |
5540000 |
|
Error Term |
21457
|
-21457
|
0
|
|
(error as % of inflows) |
0% |
-1% |
0% |
| Opening Storage capacity |
|
|
|
| - major storages |
0 |
|
0 |
| - farm dams |
0 |
|
0 |
| - other |
0 |
0 |
0 |
| Closing Storage capacity |
|
|
|
| - major storages |
0 |
|
0 |
| - farm dams |
0 |
|
0 |
| - other |
0 |
0 |
0 |
|

Figure 6 Water balance summary diagram for Roper River water management area
Outcomes from the water cycle report
The following information becomes apparent from Table 2.
- The error in the water balance was 0%; this was mainly due to the sparse nature of information.
- The runoff and outflow estimates dominated the water balance representing more than 95% of the overall balance. The Water 2010 estimates were too high for surface water flow and too low for groundwater recharge.
- Runoff figures were based upon Water 2010 and were modified by back calculation.
- Data accuracy for the groundwater / surface water interactions was low.
- Data accuracy for water use was high.
- Almost all (99%) groundwater recharge was discharged to surface water as baseflow.
- Water use was from a mix of groundwater and surface water sources.
- All extractions were from self-extracted water (e.g. catchment dams, private diversions and groundwater bores) which is not metered or well known.
- There was no effluent recycling.
- In 2004-05 the environments’ share of the total flow in the Roper River basin was 99% of total streamflow.
- Data could not be obtained for the following items in the water balance:
- Onstream minor and farm dams
- Offstream minor catchment dams
- Groundwater aquifer volume
- Soil - unsaturated zone
- River channels
- Seepage from surface water features
- Minor catchment dams
- Environmental extractions
- Groundwater discharge to Springs
- Groundwater discharge to ET
- Groundwater Stock and Domestic Use
- Aquifer flow out of entity
Download 2004-05 water cycle report:
Roper River SWMA water cycle report (100 kb)
(this document requires the use of Adobe Acrobat Reader)
Summary of data availability and reliability
The data for this water balance is highly variable with only gauging and water use information being high quality. Most of the other information is based on previous work and estimates.
The data for this water balance is predominantly category D, indicating that the majority of the data is estimated. In addition, 86% of the fields have no information for them either due to them being not applicable (e.g. conveyance losses from irrigation channels), or not available (farm dams). The overall reliability index for the catchment was ±96%.
Table 3 Summary of Roper River water management area data reliability
| A (+/- 10%) |
0 |
0 |
0.00 |
| B (+/- 25%) |
0 |
0 |
0.00 |
| C (+/- 50%) |
3 |
9370263 |
84.57 |
| D (+/- 100%) |
5 |
1709430 |
15.43 |
| E (no data) |
26 |
- |
- |
| F (no data currently available) |
0 |
- |
- |
| Not applicable |
22 |
- |
- |
|
Total |
56 |
11079693 |
|
| WMA reliability index |
±96% |
|
|
|
Water balance error (%) |
0% |
|
|
|