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Sunkoshi River

River in Nepal


River in Nepal

FieldValue
nameSunkoshi
imageThe Friendship Bridge connecting China with Nepal.jpg
image_size270px
image_captionThe Sino-Nepal Friendship Bridge over Bhote Koshi at Kodari
source1_locationChoukati, Nepal
source1_coordinates
source1_elevation2400 m
source2_locationNyalam County, Tibet
source2_coordinates
source2_elevation5300 m
mouth_locationConfluence with Arun and Tamur to form Saptkoshi at Trivenighat, Nepal
mouth_coordinates
subdivision_type1Country
subdivision_name1Tibet, Nepal
mouth_elevation640 m
river_systemKoshi River
tributaries_leftTamba Koshi, Likhu Khola, Dudh Koshi
tributaries_rightBhote Koshi, Indravati River

The Sunkoshi, also spelled Sunkosi, is a river that is part of the Koshi or Saptkoshi River system in Nepal. Sunkoshi has two source streams, one that arises within Nepal in Choukati, and the other more significant stream that flows in from Nyalam County in the Tibet region of China. The latter is called Bhote Koshi in Nepal and Matsang Tsangpo in Tibet.{{efn|An alternative Tibetan name Bö Chu (), also spelt Po Chu or Poi Chu, is also used in sources.{{Cite web | archive-url = https://web.archive.org/web/20200320020608/http://hydrologie.org/redbooks/a218/iahs_218_0319.pdf | archive-date = 20 March 2020

River course

The Sunkoshi's headwaters are located in the Zhangzangbo Glacier in Tibet. Both Sunkoshi and Bhote Koshi river courses together form one basin that covers an area of about 3394 km2.

The Indravati meets the Sunkoshi at Dolaghat, where it is followed by the Arniko Rajmarg. From there, the Sunkoshi flows eastwards through the valley formed between the Mahabharat Range and the Himalayas. The Tamakosi, Likhu, Dudhkosi, Arun and Tamor are its left tributaries and Indravati is the right tributary.

The average annual flow is 2.2 x 1010 m3. The average sediment load is 5.4 x 107 m3.

Sunkoshi river in December 2023

The Tamur and the Arun rivers join the Sunkoshi at Tribenighat to form the Saptkoshi, which flows through the Chatra Gorge across the Mahabharat Range onto the Gangetic plain.

Names and etymology

In Nepali language, the word "sun" means gold and golden; and the word "kosi" means river.

Koshi River system

The Koshi River drains eastern Nepal. It is also known as Saptkoshi River because of the seven rivers joining in east-central Nepal to form this river. The main rivers forming the Koshi River system are Sunkoshi, Indravati, Tamba Koshi, Bhote Koshi, Dudh Kosi, Arun and Tamur Rivers. The Saptkoshi River flows through the Chatra Gorge in a southerly direction into northern Bihar and joins the Ganges.

The Sunkoshi contributes about 44% of the total water of the Saptakoshi, the Arun 37% and the Tamur 19%.

Infrastructures

  • Sunkosi–Kamala multipurpose project: The Sunkoshi has a 90% reliable flow of 126 m3/s. It was proposed to divert the water from a small weir across the river near Kurule through a 16.6 km tunnel and a 61.4 MW associated powerhouse to the Kamala River, flowing through central Nepal. Some 72 m3/s of water would be transferred to the Kamala River for the irrigation and further generation of power.

Hazards

In July 1981, a sudden ice avalanche caused a Glacial Lake Outburst Flood in the moraine-dammed Zhangzangbu-Cho Lake in the headwaters of the Poiqu in Tibet. The ensuing debris flow destroyed bridges, and sections of both the Arniko and the Nepal–China highways.

On 2 August 2014, a landslide at Jure blocked the river downstream from Barabise and created a large lake that submerged a hydropower station. This huge rockslide of approximately 5000000 m3 blocked the Sunkoshi River upstream of Jure village. This landslide killed approximately 155 people and destroyed approximately 120 houses completely and 37 partially. The area was declared a flood crisis zone, and local communities were evacuated. The power supply was interrupted, and the Arniko Highway was blocked.

Water sports

The Sunkoshi is used for both rafting and intermediate kayaking. It has grade III-IV rapids. The most common put-in point of a Sunkoshi river trip is Dolaghat, at an elevation of 620 m and it ends at the Chatra Gorge at 115 m, a distance of around 272 km.

The first successful descent of the Sunkoshi was made in late September 1970 by Daniel C. Taylor, Terry Bech, Cheri Bremer-Kamp, and Carl Schiffler. They entered the river at Dolaghat and exited at the Nepal-India border. Their expedition took four days. Before this successful trip, there were four known unsuccessful attempts to descend the river, and one unsuccessful attempt to ascend the river in a jet boat under the leadership of Edmund Hillary.

Notes

References

References

  1. Shrestha, A. B., Eriksson, M., Mool, P., Ghimire, P., Mishra, B. & Khanal, N. R.. (2010). "Glacial lake outburst flood risk assessment of Sun Koshi basin, Nepal". Geomatics, Natural Hazards and Risk.
  2. Dorje, Gyurme. (2004). "Footprint Tibet Handbook with Bhutan". Footprint Handbooks.
  3. (11 November 2021). "Changes in glacial lakes in the Poiqu River basin in the central Himalayas". Hydrology and Earth System Sciences.
  4. (23 November 2020). "Contemporary Environmental Problems in Nepal: Geographic Perspectives". Springer Nature.
  5. Mool, P. K.; Joshi, S. P.; Bajracharya, S. R. (2001). Glacial Lake Outburst Floods and Damage in the Country. Pages 121–136 in: Inventory of Glaciers, Glacial Lakes and Glacial Lake Outburst Floods: Monitoring and Early Warning Systems in the Hindu Kush-Himalayan Region, Nepal. International Centre for Integrated Mountain Development, Kathmandu.
  6. Dorje, G.. (1999). "Tibet Handbook: with Bhutan". Footprint Handbooks.
  7. Kattelmann, R.. (1991). "Hydrologic regime of the Sapt Kosi basin, Nepal". Hydrology for Water Management of Large River Basins (Proceedings of the Vienna Symposium).
  8. Sharma, U. P. (1996). Ecology of the Koshi river in Nepal-India (north Bihar): a typical river ecosystem. In: Jha, P. K., Ghimire, G. P. S., Karmacharya, S. B., Baral, S. R., Lacoul, P. (eds.) Environment and biodiversity in the context of South Asia. Proceedings of the Regional Conference on Environment and Biodiversity, 7–9 March 1994, Kathmandu. Ecological Society, Kathmandu. Pp 92–99.
  9. Turner, R. L.. (1931). "A Comparative and Etymological Dictionary of the Nepali Language". K. Paul, Trench, Trubner.
  10. Turner, R. L.. (1931). "A Comparative and Etymological Dictionary of the Nepali Language". K. Paul, Trench, Trubner.
  11. Negi, S. S.. (1991). "Himalayan Rivers, Lakes, and Glaciers". Indus Publishing Company.
  12. Rao, K. L.. (1995). "India's Water Wealth". Orient Longman Ltd..
  13. Bhattarai, D.. (2009). "The Nepal–India Water Relationship: Challenges". Springer Science & Business Media.
  14. Gajurel, D.. (2004). "High Dam Planned for Nepal's Sapta Koshi River". Environment News Service.
  15. Jaboyedoff, M.. (2015). "Characterization of the Jure (Sindhupalchok, Nepal) Landslide by TLS and field investigations". European Geosciences Union.
  16. (2014). "Eye on the Sun Koshi Landslide: Monitoring and Infrastructure Planning Key to Minimizing Scale of Disasters". International Centre for Integrated Mountain Development.
  17. Woodhatch, T. (1999). Nepal Handbook. p. 167, Footprint Handbooks, Augusta {{ISBN. 0658000160
  18. Taylor-Ide, D. (1995). "Something Hidden Behind the Ranges." San Francisco: Mercury House
  19. Taylor, D. C. "Yeti: An Ecology of a Mystery." New Delhi: Oxford University Press, pp. 119-130.
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