Theewaterskloof Dam

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Theewaterskloof Dam
Theewaterskloofdam.jpg
View of Theewaterskloof reservoir from hills to the east
South Africa Western Cape relief location map.svg
Red pog.svg
Location in the Western Cape
Location Western Cape, South Africa
Coordinates 34°4′41″S19°17′21″E / 34.07806°S 19.28917°E / -34.07806; 19.28917
PurposeIrrigation and domestic
Opening date1980
Owner(s) Department of Water and Sanitation
Dam and spillways
Type of dam Earth fill dam
Impounds Sonderend River
Height35 m (115 ft)
Length646 m (2,119 ft)
Reservoir
CreatesTheewaterskloof Dam Reservoir
Total capacity480,406 Ml (16,965.4×10^6 cu ft)
Catchment area 500 km2 (190 sq mi)
Surface area5,059 ha (12,500 acres)

Theewaterskloof Dam is an earth-fill type dam located on the Sonderend River near Villiersdorp, Western Cape, South Africa. Administratively it is located within Theewaterskloof Local Municipality. It was established in 1978 and is the largest dam in the Western Cape Water Supply System with a capacity of 480 million cubic metres, about 41% of the water storage capacity available to Cape Town, which has a population of over 4 million people. [1] The dam mainly serves for municipal and industrial use as well as for irrigation purposes. The hazard potential of the dam has been ranked high (3). [2]

Contents

Dam characteristics

Theewaterskloof Dam water extraction point.jpg

Theewaterskloof Dam's earth-fill wall is 646 metres (2,119 ft) long and 35 metres (115 ft) high. [2] An inlet tower and conduit through the wall allow for releases of water into the Sonderend River. The spillway can handle a maximum flood of 394 cubic metres per second (13,900 cu ft/s). [3] The Charmaine intake tower draws water from the reservoir into the Franschhoek Tunnel, which conveys it under the Franschhoek Mountains into the Berg River catchment and ultimately into Cape Town's water supply. In winter the tunnel can operate in reverse, conveying surplus water from the Berg River into Theewaterskloof. [3] An additional intake tower supplies water to the Vyeboom Irrigation Board for irrigation of areas around the dam.

Water restrictions

Theewaterskloof at approximately 12% capacity on 10 February 2018 Theewaterskloof Dam 2018 02 10 (28425520089).jpg
Theewaterskloof at approximately 12% capacity on 10 February 2018

Below-average rainfall since 2015 have seen the Theewaterskloof water level drop to critical levels. Water restrictions were imposed by the City of Cape Town in 2016 to meet a target of 600 million litres of water per day, [4] with residents limited to 100 litres of water per day and a ban on car washing, watering gardens and topping up swimming pools with municipal water.

By the end of the 2017 dry season, Theewaterskloof had declined to a level of 12.9%, with the last 10% mostly unreachable. A storm in June 2017 brought heavy rain, increasing the level to 15%, but overall rainfall in 2017 remained very low. Media footage of the declining dam level sparked the importance of conserving water. [5] Water restrictions in Cape Town were increased from Level 4 to Level 4b on 1 July 2017, limiting consumption to 87 litres of water per person per day. Rainfall in 2017 remained well below average, and by early 2018 the dam was again approaching critically low level, resulting in water consumption being limited to only 50 litres per person per day, and plans for a possible "Day Zero" in April 2018 when Cape Town's municipal water supply was predicted to be shut off. [6]

As a result of good rains in the winters of 2019 and 2020, the Theewaterskloof water level reached 100% in October 2020. [7]

Rainfall and capacity

Theewaterskloof dam has a capacity of 480,406 megalitres (16,965.4×10^6 cu ft) of water, and when full the reservoir covers an area of 5,059 hectares (12,500 acres). [2] The catchment area of 500 square kilometres (190 sq mi) is served by streams emanating in the Hottentots Holland mountain range. This area has a long-term average of 69 days with precipitation per year. [8] Historically [9] records show we are in a dry period [10] 1mm of rain per square meter equates to 500 000 000 litres falling on this area. Hence it requires a full metre of rainfall with 100% runoff to fill the dam from totally empty, which is unlikely to happen in any single year. It takes a few days for all the runoff to reach the dam. Evaporation and how saturated the ground is affects the amount of water reaching the dam. An average amount of between 9% and 15% is used to offset the values against evaporation and soil absorption. A deeper dam has less evaporation due to less surface area per volume.

Social events

The Theewaterskloof Dam is also the home of the annual Synergy Live music festival, one of the biggest outdoor music festivals in South Africa, which typically takes place on the last weekend of November or the first weekend of December. [11]

See also

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References

  1. List of South African Dams from the Department of Water Affairs
  2. 1 2 3 "List of Registered Dams". Dam Safety Office, Department of Water and Sanitation. November 2019. Retrieved 12 August 2021.
  3. 1 2 van Vuuren, Lani (May 2011). "Blood, sweat and tears at Riviersonderend" (PDF). The Water Wheel. Water Research Commission. 10 (3): 22–25. Retrieved 12 August 2021.
  4. "Residential water restrictions explained". www.capetown.gov.za. Retrieved 2017-06-13.
  5. "Western Cape dam levels up only 1.5% after storms". www.enca.com. Retrieved 2017-06-13.
  6. Watts, Jonathan (2018-02-03). "Cape Town faces Day Zero: what happens when the city turns off the taps?". The Guardian. Retrieved 2021-03-29.
  7. Bhengu, Lwandile (4 October 2020). "Western Cape's largest dam overflows for the first time in six years". Sowetan. Retrieved 26 June 2021.
  8. institutt, NRK og Meteorologisk. "Weather statistics for Theewaterskloofdam". yr.no. Archived from the original on 2017-07-31. Retrieved 2017-07-10.
  9. "Rainfall History".[ permanent dead link ]
  10. "Western Cape rainfall". Archived from the original on 2018-01-15. Retrieved 2017-07-30.
  11. "Synergy". Synergy. 2015. Archived from the original on 15 May 2017. Retrieved 30 May 2017.