Average estimated groundwater volume in New Zealand regions
2010–2014, billion cubic metres
| Region | Billion cubic metres |
|---|---|
| Auckland | 17.88 |
| Bay of Plenty | 31.52 |
| Canterbury | 519.29 |
| Waikato | 34.54 |
| Gisborne | 1.16 |
| Hawke's Bay | 6.84 |
| Marlborough | 0.51 |
| Manawatū-Whanganui | 3.65 |
| Northland | 3.22 |
| Otago | 17.56 |
| Southland | 22.53 |
| Tasman | 9.56 |
| Taranaki | 25.13 |
| West Coast | 11.22 |
| Wellington | 4.98 |
Definitions
Groundwater: the water stored beneath Earth’s surface in aquifers (layers of water-bearing rock or sand). It is used for human and stock drinking water, irrigation, and industry, and also has a role in sustaining some rivers, lakes, and wetlands, especially during low-flow periods. The health of surface-water ecosystems also depends on groundwater.
Data provided by
Dataset name
Environmental Reporting: Average estimated groundwater volume by region 2010–2014
Webpage:
https://data.mfe.govt.nz/table/52529-average-estimated-groundwater-volume-by-region-2010-2014/
How to find the data
At URL provided, select 'Export' from the top right of the screen, and then 'Create Export'. You will have to register to download this dataset.
Import & extraction details
File as imported: Environmental Reporting: Average estimated groundwater volume by region 2010–2014
From the dataset Environmental Reporting: Average estimated groundwater volume by region 2010–2014, this data was extracted:
- Rows: 2-17
- Column: 2
- Provided: 16 data points
This data forms the table Environment - Average estimated groundwater volume by region 2010–2014.
Dataset originally released on:
September 29, 2015
Method of collection/Data provider
Groundwater volumes are based on estimates of:
- aquifer locations and extents, based on outlines described by White (2001) and Moreau and Bekele (2015)
- the depth or thickness of the aquifer, based on measurements of the winter groundwater level in at least one indicator well for each aquifer (monitored by regional councils)
- an aquifer’s porosity (how much water can be stored per volume of aquifer material; eg gravels with large spaces between pebbles can store more water than a tightly packed material without any void space).