| Click a question to show/hide the answer. General Prescribed areas To determine the status of streamflow, beginning with the 2015 reporting period, the current reporting year is analysed and compared to the total period of record available. First, annual streamflow for each streamflow gauging station is summarised for the total period of record available. Data is extended to a consistent period of record using double mass analysis for gauging stations with a shorter period of record. Next, the status for each gauging station was determined by expressing each reporting year’s streamflow in relation to the total available annual streamflow record using a percentile rank function. For prescribed areas with a single streamflow gauging station (i.e. Morambro Creek) or a streamflow gauging station at the end of the system (i.e. Barossa), which captures the total streamflow of the prescribed area, the annual streamflow percentile of that station is used to determine the status of streamflow. For prescribed areas with unconnected catchments and more than one streamflow gauging station that fails to capture the total streamflow of the prescribed area (i.e. the Eastern and Western Mount Lofty Ranges), the annual streamflow from gauging stations in hydrologically similar surface water catchments are added together and then the total combined streamflow is ranked to determine the status of streamflow. Rainfall data used in the Groundwater and salinity status reports are sourced from the latest available from the Scientific Information for Land Owners (SILO) Patched Point Dataset, which uses Bureau of Meteorology daily rainfall measurements and is available online at https://legacy.longpaddock.qld.gov.au/silo/ SILO is hosted by the Science Division of the Queensland Government's Department of Environment and Science and provides daily datasets for a range of climate variables in ready-to-use formats suitable for research and climate applications. Rainfall maps have been compiled using daily gridded data produced by the BoM Australian Water Availability Project (http://www.bom.gov.au/jsp/awap/), the aim of which is to monitor the state and trend of the terrestrial water balance of the Australian continent, using model-data fusion methods to combine both measurements and modelling. DEW maintains a database of extraction volumes from the water meters of licensed water users. These volumes are based on the best data available at the time of publication. However, some meter readings may be awaiting verification and as such, extraction data is subject to change. Stock and domestic use does not require a license and it is therefore not included in published extraction volumes. Once the annual streamflow percentile has been determine for the prescribed area, an overall status – or traffic light colour – for the regional-scale surface water resource is then assigned. Status is assigned based on the annual streamflow percentile for the current reporting period being within a percentile grouping range: - annual streamflow between the 75th‑100th percentile of the period of record (green status)
- annual streamflow between the 50th‑75th percentile of the period of record (yellow status)
- annual streamflow between the 25th‑50th percentile of the period of record (amber status)
- annual streamflow between the 0‑25th percentile of the period of record (red).
Definitions of Surface Water Status Reports’ status symbols have been updated to align with the new approach of assigning the status of prescribed surface water resources based on streamflow data only. Both suites of status symbol definitions can be viewed via the Water Resource Status Symbols link on the Water Resources Assessments page on WaterConnect. In 2014, a review of the Groundwater status reports and Surface Water status reports was undertaken with the aim of refining the existing reporting format, primarily to improve each report’s clarity and usability. Following consultation, a number of technical amendments to the reporting approach were adopted, beginning with the 2015 reporting period. There are three main changes to Groundwater Status Reports: - Assessing the status of groundwater resources is now based on five-year trends, compared to the previous approach of year-on-year snapshot reporting. This change also resulted in an update to the definitions of status symbols.
- Reporting of rainfall and groundwater extraction data over a five-year period – shown in water-use years (i.e. financial years) – thereby providing insights into possible relationships between variations in annual rainfall, changing rates of groundwater extraction and changing groundwater levels and salinity
- Including gridded rainfall charts at three different temporal scales.
There is one main change to Surface Water Status Reports: - Assessing the status for surface water resources is now based solely on streamflow data—where the status of each reporting year’s streamflow is expressed in relation to the total available annual streamflow records, using a percentile function.
To determine the status of groundwater levels, beginning with the 2015 reporting period, the trend in groundwater levels over the past five years was analysed (e.g. for 2015 reports, this is the period 2011–15 inclusive). First, each monitoring well was assigned a ‘threshold groundwater level’. This is the lowest groundwater level measured in that monitoring well over its entire data record, or the ‘historical minimum’. Next, the status for each well was determined based on the 2015 minimum water-level measurement and the trend in water level over the past five years, specifically: (1) if the 2015 minimum groundwater level is greater than the historical minimum, the status is assigned according to whether the trend is rising (blue), declining (yellow) or the water level is stable (green); or (2) if the 2015 minimum groundwater level is the lowest on record, the status is assigned according to whether the trend is rising (purple), declining (black), or the water level is stable (grey). For the purpose of Groundwater status reports, the definition of a ‘stable’ water level is based on tolerances, whereby a well’s groundwater level can show a rising or declining trend, but measure within a certain margin (tolerance) and still be considered stable. These tolerances vary with aquifer type and the scale of the resource. This approach was taken to: (1) accommodate wells that show water levels with such low rates of water level rise or decline that they can be considered stable; and (2) account for very small errors (e.g. human or instrument error) that are common in measurements of any kind, including water levels. The tolerances that have been chosen to demarcate a stable water level are based on the trend (i.e. rate of change) in water level over the past five years. For sedimentary systems—i.e. for both regional confined systems with large storages; and for moderately sized unconfined and semi-confined to confined aquifers—the tolerance chosen to delineate stable water levels is 0.02 m/y. Fractured rock aquifers have generally lower storages and are assigned a tolerance of ±0.01 m/y. Smaller unconfined lenses in the Eyre Peninsula are assigned a tolerance of ± 0.004 m/y. To determine the status of groundwater salinity for the 2015 reporting period, the trend in groundwater salinity over the past five years was analysed (e.g. for 2015 reports, this is the period 2011–15 inclusive). The status for each well is then determined, based on whether the trend in salinity is either declining (blue), rising (yellow) or stable (green). In a similar approach to that taken for groundwater levels, the definition of ‘stable’ salinity is based on tolerances, whereby a well’s groundwater salinity can show a rising or declining trend, but measure within a certain margin (tolerance) and still be considered stable. The tolerance chosen to delineate stable salinity is ±10%, measured over the past five years:
∆S = [(five-year trend / S2011) x
100 (%)] where
∆S is the change in salinity [%]; five-year trend is the trend calculated over the past five years (2011–15 inclusive) [mg/L]; and
S2011 is the average salinity measured in 2011 [mg/L]. A tolerance of ±10% was chosen to account for errors in measuring groundwater salinity (e.g. human or instrument error) and to compensate for possible errors due to: - timing of sample collection (i.e. seasonal differences such as winter versus summer)
- inconsistencies in purging of wells before the salinity sample is collected
- temperature effects
- calibration of instruments.
Once the groundwater level and salinity status has been assigned for each well, an overall status for the regional-scale groundwater resource is then assigned, and this overall status is typically based on five-year trends, as shown by the majority of monitoring wells. However, other factors are often taken into consideration, such as: the ‘robustness’ of an aquifer; rates and intensity of groundwater extraction; and the value or end-use purpose of the water (e.g. water for critical human needs). If trends in groundwater level and salinity are conflicting, a conservative approach is generally adhered to. For example, if groundwater levels are declining but salinity is stable, then the overall status will likely be based on trends in groundwater levels. Definitions of Groundwater status reports’ status symbols have been updated to align with the new approach of assigning the status of groundwater resources based on past five-year trends (in contrast to year-on-year snapshot reporting). Both suites of status symbol definitions can be viewed via the Water Resource Status Symbols link on the Water Resources Assessments page on WaterConnect. The prescribed area status reports provide the community with factual information and analysis of the available groundwater and surface water data. They provide a snapshot of the current status of prescribed water resources to assist the government, water resource users, and the community to plan and manage prescribed water resources into the future. Prescribed area status reports are being prepared for Prescribed Water Resource Areas, Prescribed Wells Areas, and a limited number of important areas which have adequate monitoring data available to assess the status of the prescribed water resources. The reports are prepared using the latest data available to the Department of Environment, Water and Natural Resources (the Department). Most of the data used to create the reports are collected by the Department through metering of licensed water users, and through regular monitoring of the Department's streamflow and Observation Well network. Observation Well data can be accessed from the
Groundwater Data application. Surface water data can be accessed from the
Real-Time Water Data application. There are many reasons why the status of a prescribed water resource may have changed. Prescribed Area Assessment Reports are prepared using the best information and scientific knowledge available at the time of preparation. New knowledge obtained may have revealed a change in the water resource data, or availability to existing users. When the decision was made to prepare Groundwater Status Reports in the new format (Summary Report Card), several of the 2011 status reports were already completed and it would have caused unnecessary delays in the release of these reports if they were changed to the new format. Refer to “Why was the format of the Groundwater Status Reports changed?” Those parts of the environment, the species composition and natural ecological processes, which are determined by the temporary or permanent presence of flowing or standing water, above or below ground. The in-stream areas of rivers, riparian vegetation, springs, wetlands, floodplains, estuaries and lakes are all WDEs). To clearly and accurately communicate the salinity of the resource for a particular year, it is best to view the latest salinity reading for the particular year recorded for a salinity monitoring well. Whilst regional salinity contours are useful in viewing regional salinity variability, the use of the latest salinity for the year is appropriate to indicate the specific salinity at a particular point in time. The regional salinity contours will still be communicated in the technical reports, which are to be prepared every 5 to 10 years (also refer to “Why was the format of the Groundwater Status Reports changed?”). Where over-use of water resources is identified, the resources can be prescribed under the Natural Resources Management Act 2004. This means a regulatory framework can be introduced to ensure the resource is managed sustainably. Once a water resource is prescribed the relevant regional Natural Resources Management Board must prepare a draft Water Allocation Plan. Community consultation is a key aspect in the preparation of Water Allocation Plans. Water Allocation Plans and related information are published on regional NRM Board websites. (Access your regional NRM Board website from
www.nrm.sa.gov.au). The Department also prepares regional Demand and Supply Statements for each region of South Australia. These provide a long-term view of all water sources and demands across South Australia's eight Natural Resources Management regions. Send an email to the Department of Environment, Water and Natural Resources Groundwater Team at
DEWNRGroundwater@sa.gov.au and we will respond to your query as quickly as possible. Or, contact the Department of Environment, Water and Natural Resources (DEWNR) on (08) 8463 6800. After the release of the base reports and in consultation with stakeholders, it was decided that the Groundwater Summary Report Cards could be more efficiently and effectively provided by focusing solely on the significant aquifers within each prescribed area, in particular, the primary aquifers from which the majority of licensed groundwater extractions are taken. You can access up-to-date monitoring data for the remaining groundwater resources from the Groundwater Data application under the Data Systems tab on this website. Non-prescribed regions Frequently Asked Questions Top | |