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Database Title |
14.2 Hydrometric Database |
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| Keywords Type1. Type 11. |
Freshwater, water quantity |
| Abstract | The Hydrometric Database provides time series of water level river flow data collected from New Zealand's national river flow network (National Hydrometric Network). The database also stores related hydrological time series data such as rainfall amounts and river sediment concentrates. New Zealand's hydrometric data collection began in the early 1900s when lake levels began to be monitored for hydro electric potential. Major rivers of regional importance were monitored regularly from the 1930s. During the international hydrological decade (1965-1974) monitoring started at over 50 of 90 representative river catchments. The representative water- level recording stations were operated primarily by the Ministry of Works and Development (later DSIR). Stations were also run by regional water boards. By 1990 more than 500 water level recorders were operating either as part of the DSIR national network (290 stations for scientific and commercial purposes) or as part of local networks run by regional councils (for purposes such as water resource allocation or flood warning). In 1994 a reduction in funding required NIWA (which had inherited the hydrological network from the former DSIR) to reduce the number of stations by 20 percent. Stations were classified as follows:
As a number of stations were selected for more than one class a total of 230 stations were selected to operate from 1994 onwards as part of the national network. Regional councils also collect flow data. This data is contributed to the national database on a reciprocal sharing arrangement for 10 regional councils. |
| Geographical Coverage | New Zealand |
| Dataset start date. | 1905 |
| Dataset end date. | Current |
| Status/currency. | In progress |
| Update frequency. | Every 15 minutes |
| Maintenance. | Much of the data collection is funded by FRST. Data is also collected by commercial users, especially the hydro electric industry. |
Technical Evaluation |
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| Parameters- what is measured | Water levels |
| Parameters- what is calculated | Water flows |
| Methods used to measure parameters | The water level at each recording site is measured automatically at 15 minutes intervals. The flow rate is determined by the use of a water level-flow rating curve. As the relationship between water level and flow changes over time this needs to be calibrated regularly (monthly) at each site. |
| Secondary sources of data | N/A |
| Scale of use. | 230 sites |
| Number of records | >2 billion |
| GIS compatibility. | Because there is so much data it is not yet possible to have true GIS interface for water quantity data. This is being worked on. |
| Available formats for users. | Data is in Tideda software. As many users have this software data is often made available on a Tideda file. Monthly mean flows are available as Excel or text files. |
| Access constraints. | There are restrictions on the commercial data. Permission is needed from the funder of commercial data. |
| Measurement Accuracy | To be completed by database manager. |
| Completeness of dataset | To be completed by database manager. |
| Positional accuracy | To be completed by database manager. |
| Database steward | NIWA |
| Database custodian | NIWA |
| Database custodian contact person | Charles Pearson; Kathy Walter |
| Database custodian Contact Address Phone Fax |
P.O. Box 80622 Christchurch +64 3 348 8987 +64 3 348 5548 c.pearson@niwa.cri.nz ; k.walter@niwa.cri.nz |
| References | Pearson, C.P. 1998. Changes to New Zealand National hydrometric network in the 1990s. Journal of hydrology(New Zealand) 37 (1); 1-17. |
| Date metadata record prepared. | October 1999 |
| Author of metadata record. | Victoria Froude |
Management Evaluation |
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| Original purpose. | The first sites were established to collect information for hydro electric purposes. |
| Relationships with classification systems. | N/A |
| Relationships with other databases | This database is part of the Water Resources Archive. There are close links with the national climate database. It is used in association with other databases to develop models about land use and water quantity. |
| Known relationships with proposed EPIP indicators. | N/A |
| Who uses this database? |
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| Public awareness of the database | There have been some articles in popular publications. |
| Database strengths. |
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| Database limitations. |
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What are the Current and Emerging Uses of the Database for: |
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| Assisting with determining historic state/baseline. | The database is useful for determining historic baselines, e.g. flood frequency and magnitude, low flow level and frequency. |
| Assisting with determining current state/baseline. | The database provides real time data for water levels and flows. |
| Assisting with modeling possible future outcomes. | The database is used, often in association with other databases, for a considerable amount of modeling work. |
| Risk assessment. | The database is used extensively to assess risk, e.g. flood and low flow risk. |
| Monitoring site selection and sample design. | While the database originally developed on an ad hoc basis, a reduction in the number of sites monitored was done in a systematic way. It may be possible to use the database as part of a different monitoring programme, depending on what type of information is sought. |
| Aggregating and reporting data locally, regionally or nationally. | Internal and quarterly reports are produced. There is also an annual report for each recording station (required as part of Telarc accreditation). Information can be provided by Region. |