Sunkoshi River
The Sunkoshi, also called Sunkosi, is a trans-boundary river that originates in Tibet Autonomous Region and is part of the Koshi or Saptkoshi River system in Nepal.[1]
Sunkoshi | |
---|---|
The Sino-Nepal Friendship Bridge over the Sunkoshi at Kodari | |
Location | |
Country | Tibet, Nepal |
Physical characteristics | |
Source | |
• location | Tibet |
• elevation | 8,012 m (26,286 ft) |
Mouth | |
• location | Confluence with Arun and Tamur to form Saptkoshi at Trivenighat, Nepal |
• coordinates | 26°54′47″N 87°09′25″E |
• elevation | 640 m (2,100 ft)[1] |
Basin features | |
River system | Koshi River |
Tributaries | |
• left | Tamba Koshi, Likhu Khola, Dudh Koshi |
• right | Indravati River |
River course
The Sunkoshi's headwaters are located in the Zhangzangbo Glacier in Tibet.[2] Its upper course, the Bhote Koshi, is known as Poiqu in Tibet.[3] Both river courses together form one basin that covers an area of about 3,394 km2 (1,310 sq mi).[1]
The Indravati meets the Sunkoshi at Dolaghat, up to where it is followed by the Arniko Rajmarg.[4] From there, the Sunkoshi flows eastwards through the valley formed between the Mahabharat Range and the Himalayas.[1] Tamakosi, Likhu, Dudhkosi, Arun and Tamor are its left tributaries and Indravati is the right tributary.
The average annual flow is 22 x 109 m3. The average sediment load is 54 x 106 m3.[5]
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 on to the Gangetic plain.[6] There are few more smaller tributaries of the Sunkoshi such as Rosi Khola, Junga Khola, and Sapsu Khola.
Names and etymology
Nepali: सुनकोशी
In Nepali language, the word "sun" means gold and golden;[7] and the word "kosi" means river.[8]
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.[6][9]
The Sunkoshi contributes about 44% of the total water of the Saptakoshi, the Arun 37% and the Tamur 19%.[10]
Infrastructures
- Sunkosi–Kamala multipurpose project: The Sunkoshi has a 90% reliable flow of 126 cubic metres per second (4,400 cu ft/s). It was proposed to divert the water from a small weir across the river near Kurule through a 16.6 km (10.3 mi) tunnel and a 61.4 MW associated power house to the Kamala River, flowing through central Nepal. Some 72 cubic metres per second (2,500 cu ft/s) of water would be transferred to the Kamala River for the purposes of irrigation and further generation of power.[11][12]
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.[2]
On 2 August 2014, a landslide blocked the river downstream from Barabise and created a large lake that submerged a hydropower station. The collapsed river bed buried several houses, more than 30 people died. The area has been declared a flood crisis zone, and local communities are evacuated. Power supply is interrupted, and the Arniko Highway blocked.[13] See also 2014 Sunkoshi blockage
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 (2,030 ft) and it ends at the Chatra Gorge at 115 m (377 ft), a distance of around 272 km (169 mi).[14]
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.[15] Prior to this successful trip, there are 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.[16]
References
- 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. 1 (2): 157–169. doi:10.1080/19475701003668968. S2CID 129446680.CS1 maint: multiple names: authors list (link)
- 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.
- Yamada, T., Sharma, C. K. (1993). Glacier lakes and outburst floods in the Nepal Himalaya. IAHS Publications-Publications of the International Association of Hydrological Sciences, 218: 319–330.
- Dorje, G. (1999). Tibet Handbook: with Bhutan. Bath: Footprint Handbooks. ISBN 9781900949330.
- Kattelmann, R. (1991). "Hydrologic regime of the Sapt Kosi basin, Nepal" (PDF). Hydrology for Water Management of Large River Basins (Proceedings of the Vienna Symposium). 201: 139–148.
- 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.
- Turner, R. L. (1931). "sun". A Comparative and Etymological Dictionary of the Nepali Language. K. Paul, Trench, Trubner, London.
- Turner, R. L. (1931). "kosi". A Comparative and Etymological Dictionary of the Nepali Language. K. Paul, Trench, Trubner, London.
- Negi, S. S. (1991). "Kosi River System". Himalayan Rivers, Lakes, and Glaciers. New Delhi: Indus Publishing Company. pp. 89–90. ISBN 9788185182612.
- Rao, K. L. (1995). India's Water Wealth. Hyderabad: Orient Longman Ltd. p. 70. ISBN 9788125007043.
- Bhattarai, D. (2009). "Sunkosi–Kamala Multi–purpose Project". In Dhungel, D. N.; Pun, S. B. (eds.). The Nepal–India Water Relationship: Challenges. Springer Science & Business Media. pp. 92–93. ISBN 9781402084034.
- Gajurel, D. (2004). "High Dam Planned for Nepal's Sapta Koshi River". Environment News Service. Retrieved 14 May 2010.
- Shrestha, A. B., Khanal, N. R., Shrestha, M., Nibanupudi, H. K. and Molden, D. (2014). Eye on the Sun Koshi Landslide: Monitoring and Infrastructure Planning Key to Minimizing Scale of Disasters. International Centre for Integrated Mountain Development, Kathmandu.
- Woodhatch, T. (1999). Nepal Handbook. p. 167, Footprint Handbooks, Augusta ISBN 0658000160
- Taylor-Ide, D. (1995). "Something Hidden Behind the Ranges." San Francisco: Mercury House
- Taylor, D. C. "Yeti: An Ecology of a Mystery." New Delhi: Oxford University Press, pp. 119-130.