Waitaki River

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Waitaki
ISS Waitaki River, Canterbury and Otago.jpg
Lower Waitaki River pictured from the International Space Station
NZ-Waitaki R.png
The Waitaki River system
Location
CountryNew Zealand
RegionCanterbury, Otago
DistrictWaimate, Waitaki
CitiesOtematata, Kurow, Duntroon, Glenavy
Physical characteristics
SourceSouthern Alps
 - locationLake Benmore, New Zealand
 - coordinates44°21′S 170°12′E / 44.350°S 170.200°E / -44.350; 170.200
Source confluenceOhau River and Tekapo Rivers
MouthPacific Ocean
 - location
New Zealand
 - coordinates
44°57′S 171°09′E / 44.950°S 171.150°E / -44.950; 171.150Coordinates: 44°57′S 171°09′E / 44.950°S 171.150°E / -44.950; 171.150
 - elevation
0 m (0 ft)
Length209 km (130 mi)
Discharge 
 - locationKurow
 - average356 m3/s (12,600 cu ft/s)
Basin features
Tributaries 
 - leftAhuriri, Otematata, Maerewhenua
 - rightHakataramea

The Waitaki River is a large braided river that drains the Mackenzie Basin and runs some 110 kilometres (68 mi) south-east to enter the Pacific Ocean between Timaru and Oamaru on the east coast of the South Island of New Zealand. It starts at the confluence of the Ohau River and the Tekapo River, now in the head of the artificial Lake Benmore, these rivers being fed by three large glacial lakes, Pukaki, Tekapo, and Ohau. The Waitaki flows through Lake Benmore, Lake Aviemore and Lake Waitaki, these lakes being contained by hydroelectric dams, Benmore Dam, Aviemore Dam and Waitaki Dam.[1] The Waitaki has several tributaries, notably the Ahuriri River and the Hakataramea River. It passes Kurow and Glenavy before entering the Pacific Ocean.

The river’s flow is normally low in winter, with flows increasing in spring when the snow cloaking the Southern Alps begins to melt, with flows throughout the summer being rainfall dependent and then declining in the autumn as the colder weather begins to freeze the smaller streams and streams which feed the catchment. The median flow of the Waitaki River at Kurow is 356 cubic metres per second (12,600 cu ft/s).[2]

The middle of the river bed formed a traditional political boundary between Canterbury and Otago. As such, the term "South of the Waitaki" is often used to refer to the Otago and Southland regions as one common area (the two regions share historical and ethnic relationships which make them distinct from the regions to the north of them).

The river is popular for recreational fishing and jetboating.

Electricity generation[edit]

The river is the site of many hydroelectricity projects.

The Waitaki dam was built first, between 1928 and 1934, and without earth-moving machinery, followed by the development of the Aviemore Dam, creating Lake Aviemore - and Benmore Dam, creating Lake Benmore. Lake Pukaki was initially dammed at this stage to provide storage and flow control. A small station was also installed on Lake Tekapo, with water taken through a 1.6 km (1 mi) tunnel to a powerstation below the level of the lake.

The original Waitaki power stations discharge water back into the Waitaki River which then forms a storage lake for the next station in the chain. The three power stations are (capacity) (annual output) (commissioned)

  • Waitaki (105 MW) (500 GWh) 1935
  • Benmore (540 MW) (2,200 GWh) 1965
  • Aviemore (220 MW) (940 GWh) 1968

In the 1960s, work was started on the Upper Waitaki project. This project consisted of taking the discharge from the original Tekapo (A) station through the Tekapo Canal, to Tekapo B station at the edge of Lake Pukaki. The dam at Pukaki was increased in height. Water from Pukaki is then transferred into the Pukaki Canal which meets the Ohau Canal from Lake Ohau into Ohau A station and Lake Ruataniwha. The Ohau Canal continues beyond Lake Ruataniwha to Ohau B midway along, before emptying through Ohau C into Lake Benmore.

Tekapo Canal

The stations are (capacity) (annual output) (commissioned)

  • Tekapo A (25 MW) (160 GWh) 1955
  • Tekapo B (160 MW) (800 GWh) 1977
  • Ohau A (264 MW) (1150 GWh) 1980
  • Ohau B (212 MW) (970 GWh) 1984/1985
  • Ohau C (212 MW) (970 GWh) 1984/1985

Later proposals[edit]

In 2001 a proposal for a new series of canals and dams was made by Meridian Energy for irrigation and electricity generation on the river.[3] This scheme, known as Project Aqua, planned to divert up to 77 percent of the lower river's flow to create a hydroelectric scheme, but these plans were dropped in March 2004. Lack of commercial viability was given as the major reason for the scheme's shelving, although strenuous public protest may also have been a major contributing factor.[4] A more modest successor scheme, the North Bank tunnel looked likely to proceed, with water rights being granted in 2009,[5] but land access negotiations were suspended in January 2013 due to flat demand for electricity forecast for the next five years.

See also[edit]

References[edit]

  1. ^ Waitaki River, An Encyclopaedia of New Zealand, edited by A. H. McLintock, originally published in 1966. Te Ara - The Encyclopedia of New Zealand, updated 26-Sep-2006.
  2. ^ Waitaki Catchment Hydrological Information, Table 3.2 Waitaki Catchment - Flow Statistics at Flow Recording Sites, February 2005, Ref. ME582, Ministry for the Environment website, retrieved 22 November 2007.
  3. ^ Braddell, Richard (14 April 2001). "Meridian overturns conventional wisdom on hydro costs". The New Zealand Herald. Retrieved 1 December 2011.
  4. ^ Cumming, Geoff (3 April 2004). "Who killed Project Aqua?". New Zealand Herald. Retrieved 9 April 2017.
  5. ^ Cogle, Fleur (26 September 2009). "Meridian wins water rights for hydro project". Timaru Herald. Retrieved 26 September 2009.

Further reading[edit]

  • Nordmeyer, Arnold (1981). Waitaki – The River and its Lakes, The Land and its People. Waitaki Lakes Committee. pp. 169 pages. ISBN 0-473-00080-6.

External links[edit]