Koshi River
The Koshi or Kosi River drains the northern slopes of the Himalayas in Tibet and the southern slopes in Nepal. From a major confluence of tributaries north of the Chatra Gorge onwards, the Koshi River is also known as Saptakoshi for its seven upper tributaries. These include the Tamor River originating from the Kanchenjunga area in the east and Arun River and Sun Koshi from Tibet. The Sun Koshi's tributaries from east to west are Dudh Koshi, Bhote Koshi, Tamakoshi River, Likhu Khola and Indravati. The Saptakoshi crosses into northern Bihar where it branches into distributaries before joining the Ganges near Kursela in Katihar district.
The Koshi is long and drains an area of about in Tibet, Nepal and Bihar. In the past, several authors proposed that the river has shifted its course for more than from east to west during the last 200 years. But a review of 28 historical maps dating 1760 to 1960 revealed a slight eastward shift for a long duration, and that the shifting was random and oscillating in nature.
The river basin is surrounded by ridges which separate it from the Yarlung Tsangpo River in the north, the Gandaki in the west and the Mahananda in the east. The river is joined by major tributaries in the Mahabharat Range approximately north of the Indo-Nepal border. Below the Siwaliks, the river has built up a megafan some in extent, breaking into more than 12 distinct channels, all with shifting courses due to flooding. Kamalā, Bāgmati and Budhi Gandak are major tributaries of Koshi in India, besides minor tributaries such as Bhutahi Balān.
Its unstable nature has been attributed to the heavy silt it carries during the monsoon season and flooding in India has extreme effects. Fishing is an important enterprise on the river but fishing resources are being depleted and youth are leaving for other areas of work.
Geography
The Koshi River catchment covers six geological and climatic belts varying in altitude from above to comprising the Tibetan plateau, the Himalayas, the Himalayan mid-hill belt, the Mahabharat Range, the Siwalik Hills and the Terai. The Dudh-Koshi sub-basin alone consists of 36 glaciers and 296 glacier lakes.The Koshi River basin borders the Tsangpo River basin in the north, the Mahananda River basin in the east, the Ganges Basin in the south and the Gandaki River basin in the west. The eight tributaries of the basin upstream the Chatra Gorge include from east to west:
- Tamur River with an area of in eastern Nepal;
- Arun River with an area of, most of which is in Tibet;
- Sun Koshi with an area of in Nepal and its northern tributaries Dudh Koshi, Likhu Khola, Tama Koshi, Bhote Koshi and Indravati.
Peaks located in the basin include Mount Everest, Kangchenjunga, Lhotse, Makalu, Cho Oyu and Shishapangma. The Bagmati river sub-basin forms the south-western portion of the overall Koshi basin.
The Dudh Koshi joins the Sun Koshi near the Nepalese village of Harkapur. At in Nepal it emerges from the mountains and becomes the Koshi. After flowing another it crosses into Bihar, India, near Bhimnagar and after another joins the Ganges near Kursela.
The Koshi alluvial fan is one of the largest in the world. It shows evidence of lateral channel shifting exceeding during the past 250 years, via at least twelve major channels. The river, which flowed near Purnea in the 18th century, now flows west of Saharsa. A satellite image shows old channels with a confluence before 1731 with the Mahananda River north of Lava.
Floods
The Koshi River is known as the "Sorrow of Bihar" as the annual floods affect about of fertile agricultural lands thereby disturbing the rural economy.The Koshi has an average water flow of. During floods, it increases to as much as 18 times the average. The greatest recorded flood was on 24 August 1954. The Koshi Barrage has been designed for a peak flood of.
Extensive soil erosion and landslides in its upper catchment have produced a silt yield of about 19 m3/ha/year, one of the highest in the world. Of major tributaries, the Arun brings the greatest amount of coarse silt in proportion to its total sediment load. The river transports sediment down the steep gradients and narrow gorges in the mountains and foothills where the gradient is at least ten metres per km. On the plains beyond Chatra, the gradient falls below one metre per km to as little as 6 cm per km as the river approaches the Ganges. Current slows and the sediment load settles out of the water and is deposited on an immense alluvial fan that has grown to an area of about 15 000 km2. This fan extends some 180 km from its apex where it leaves the foothills, across the international border into Bihar state and on to the Ganges. The river has numerous interlacing channels that shift laterally over the fan from time to time. Without channelisation, floods spread out very widely. The record flow of 24 200 m3/s is equivalent to water a metre deep and more than 24 km wide, flowing at one metre per second.
The Koshi's alluvial fan has fertile soil and abundant groundwater in a part of the world where agricultural land is in great demand. Subsistence farmers balance the threat of starvation with that of floods. As a result, the flood-prone area is densely populated and subject to heavy loss of life. India has more flood deaths than any country except Bangladesh.
2008 flood in Bihar
On 18 August 2008, the Koshi river picked up an old channel it had abandoned over 100 years previously near the border with Nepal and India. Approximately 2.7 million people were affected as the river broke its embankment at Kusaha in Nepal, submerging several districts of Nepal and India. 95% of the Koshi's water flowed through the new course. The worst affected districts included Supaul, Araria, Saharsa, Madhepura, Purnia, Katihar, parts of Khagaria and northern parts of Bhagalpur, as well as adjoining regions of Nepal. Relief work was carried out with Indian Air Force helicopters by dropping relief materials from Purnia in the worst hit districts where nearly two million persons were trapped.The magnitude of deaths or destruction were hard to estimate, as the affected areas were inaccessible. 150 people were reported washed away in a single incident. Another news item stated that 42 people had died.
The Government of Bihar convened a technical committee, headed by a retired engineer-in-chief of the water resource department to supervise the restoration work and close the breach in the East Koshi afflux embankment. Indian authorities worked to prevent widening of the breach, and channels were to be dug to direct the water back to the main river bed.
The fury of the Koshi river left at least 2.5 million people marooned in eight districts and inundated 650 km2. The prime Minister of India declared it a national calamity. The Indian Army, National Disaster Response Force and non-government organizations operated the biggest flood rescue operation in India in more than 50 years.
Glaciers, glacier lakes and outburst floods
In the Himalayas, glaciers are melting and retreating, which produces lakes insecurely dammed by ice or moraines. These dams are at risk of breaking, causing a Glacial Lake Outburst Flood with flows as great as 10,000 cubic metres a second.In the past two decades GLOF has become a topic of intense discussion within the development community in Nepal. The Dig Tsho GLOF on 4 August 1985, completely destroyed the nearly completed Namche hydropower plant and all bridges, trails, cultivation fields, houses and livestock along its path to the confluence of the Dudh-Koshi and the Sun-Koshi rivers over. The Dig Tsho glacier is on the terminus of the Langmoche Glacier. This event brought into focus the seriousness of such events and the studies to assess the glaciers, glacier lakes and GLOF followed.
Studies of the glaciers and glacier lakes were carried out in 1988 by a joint Sino-Nepalese team. The Arun-Koshi river basin hosts 737 glaciers and 229 glacier lakes, out of which 24 lakes are potentially dangerous. The Sun-Koshi basin is home to 45 glacier lakes, of which 10 are potentially dangerous. According to a Sino-Nepalese study, since the 1940s on at least 10 occasions, glacier lakes burst their dams. Among them were five bursts in three glacier lakes in the Arun River Basin and four in three glacier lakes of the Sun Koshi River Basin.
Development scenario
Multipurpose projects
The National Flood Control Policy in 1954 planned to control floods through a series of dams, embankments and river training works. The Koshi project was thus conceptualized, in three continuous interlinked stages – the first was a barrage to anchor the river that had migrated about westward in the last 250 years laying waste to a huge tract in north Bihar and to provide irrigation and power benefits to Nepal and India. The second part was to build embankments both below and above the barrage to hold the river within the defined channel. The third part envisaged a high multipurpose dam within Nepal at Barakshetra to provide a substantial flood cushion along with large irrigation and power benefits to both countries. This was followed by the Koshi Agreement between Nepal and India signed on 25 April 1954 and revised on 19 December 1966 to address Nepal's concerns. Further letters of Exchange to the Agreement between the two countries identified additional schemes for providing benefits of irrigation. While the first two parts of the plan were implemented by the Government of India, the Koshi High dam, the linchpin of the whole plan, for various political reasons has yet precluded any action for several years but has since been revived under a fresh agreement, in a modified form for further investigations and studies.Koshi barrage and irrigation
, also called Bhimnagar Barrage, was built between 1959 and 1963 and straddles the Indo-Nepal border. It is an irrigation, flood control and hydropower generation project on the Koshi River built under a bilateral agreement between Nepal and India: the entire cost of the project was borne by India. The catchment area of the river is in Nepal at the barrage site. The highest peaks lie in its catchment. About 10% is snow-fed. The Eastern Canal and the Western Canal taking off from the barrage, were designed for a discharge capacity of to irrigate and to irrigate, respectively. A hydropower plant has been built on the Eastern Canal, at a canal drop, to generate 20 MW. The Western Koshi Canal provides irrigation to in Nepal. A valuable bridge over the barrage opened up the East-West highway in the eastern sector of Nepal.An inundation canal taking off at Chatra, where the Koshi debouches into the plains, has been built to irrigate a gross area of 860 km2 in Nepal. The project was renovated with IDA assistance after Nepal took over the project in 1976.
Koshi embankment system
The Koshi barrage, with earth dams across the river, as well as afflux bunds and embankments above and below the river, confines the river to flow within embankments. Embankments on both sides downstream of the barrage with a length of were constructed to check the westward movement of the river. The embankments have been kept far apart, about 12 to, to serve as a silt trap.Sapta Koshi High Multipurpose Project (Indo-Nepal)
The governments of India and Nepal agreed to conduct joint investigations and other studies for the preparation of a detailed project report of Sapta Koshi High Dam Multipurpose Project and Sun Koshi Storage-cum-Diversion Scheme to meet the objectives of both countries for development of hydropower, irrigation, flood control and management and navigation. As currently outlined, the dam would displace approximately 75,000 people.Envisaged are a high concrete or rock-filled dam, a barrage, and two canals. The dam is on the Sapta Koshi River with an underground powerhouse, producing 3,000 MW at 50% load factor. The barrage is planned for the Sapta Koshi about downstream of Sapta Koshi High Dam to re-regulate the diverted water. The Eastern Chhatra Canal and Western Chhatra Canal, off-take from the barrage site to provide water for irrigation both in Nepal and India and navigation through Koshi up to Kursela and also in the reservoir of Sapta Koshi dam.
A power canal existing Koshi barrage at Hanuman Nagar is proposed for conveying water for irrigation from the Eastern Chatra Canal and also water that may be required downstream for navigation. To utilize the head available between Chatra and Hanuman Nagar barrages for power generation, three canal power houses, each of 100 MW installed capacity are proposed on the power canal.
Extra storage capacity of Sapta Koshi High Dam would be provided to moderate downstream flooding.
Chatra Canal System would provide irrigation to large areas in Nepal and India.
A Joint Project Office has been set up in Nepal for investigation of the project.
Hydropower
Nepal has a total estimated potential of 83,290 MW with economically exploitable potential of 42,140 MW. The Koshi river basin contributes 22,350 MW of this potential including 360 MW from small schemes and 18750 MW from major schemes. The economically exploitable potential is assessed as 10,860 MW.Adventure sports
From Kathmandu, a road crosses four major tributaries of the Koshi and reaches trekking paths to Mt Everest. Namche Bazar near the Tibetan border in Nepal is the major tourist centre in the mountainous part of the Koshi belt. Birātnagar in Nepal and Saharsa, Purnia and Katihar in India are major cities on the Koshi Plains. Kamlā, Bāghmati and Budhi Gandak are major tributaries of Koshi in India.River rafting
Commercial river rafting, also known as whitewater rafting, and canyoning is available on the Sun Koshi river and tributaries. Sun Koshi has challenging rapid grades of class 4–5.Fishing
is widely distributed in Himalayan rivers up to altitude and also inhabits the Koshi River and its tributaries.Cultural significance
The Koshi was also called Kausika in Rigveda, Nepal and Bihar in northern India. It is a major tributary of the Ganges. One major tributary of the Koshi is the Arun, much of whose course is in Tibet. This river is mentioned in the epic 'Mahabharata' as Kausiki. Seven Koshis join together to form the 'Saptakoshi River,' or 'Sapt Koshi,' which is popularly known as the Koshi.Formerly known as 'Kausiki,' named after the sage Viśvāmitra, who is said to have attained the status of Vedic or 'Rishi' on the banks of the river. Viśvāmitra was a descendant of the sage Kusika. Viśvāmitra is credited with writing many well-known Vedic Hymns on the Banks of the Koshi where he had his hermitage — The Mandala 3, the Rigveda, and the Gāyatrī Mantra. The Gāyatrī Mantra is a highly revered mantra based on a Vedic Sanskrit verse from a hymn of the Rigveda.
The mantra is named for its vedic gāyatrī metre as:
- the verse can be interpreted to invoke the deva Savitr, it is often called Sāvitrī
- recitation is traditionally preceded by oṃ and the formula bhūr bhuvaḥ svaḥ, known as the mahāvyāhṛti. The Gayatri Mantra is repeated and cited very widely in vedic literature,
- this is praised in several well-known classical Hindu texts such as the Manusmṛti, Harivamsa and Bhagavad Gita.
According to Mahabharata epic, the God of death took the form of a woman and resides on the banks of the river to limit population growth. Koshi resonates with the folklore of Mithila. The most important depictions of Koshi folklore are Koshi as a virgin absolutely care free and full of energy and as a frustrated wife of old hermit Richeek wandering in the Himalayas. Koshi is also invoked as the mother - 'Koshi Ma'. These images capture the contradiction that is inherent in the Koshi River as a source of life and death, prosperity and destruction; a mother and an enchanting virgin.
It is also the lifeline of the 'Mithila' region, today spread over more than half of India's state of 'Bihar'. It is the subject of legend and folklore of the region; the legend of Mithila extends over many centuries. Mithila is also the name of a style of 'Hindu art' created in the area.
Protected areas
In Nepal two protected areas are located in the Koshi River basin.Sagarmatha National Park
The Sagarmatha National Park encompasses the upper catchments of the Dudh Koshi River system. The park covers an area of and ranges in elevation from to at the summit of Mount Everest. Established in 1976 the park was declared a UNESCO World Heritage Site in 1979. The landscape in the park is rugged consisting of mountain peaks, glaciers, rivers, lakes, forests, alpine scrubs and meadows. The forests comprise stands of oak, blue pine, fir, birch, juniper and rhododendron. The park provides habitat for snow leopards, red pandas, musk deer, Himalayan tahrs, and 208 bird species including impeyan pheasant, bearded vulture, snow cock, and the yellow-billed chough.About 3500 Sherpa people live in villages and seasonal settlements situated along the main tourist trails. Tourism to the region began in the early 1960s. In 2003, about 19,000 tourists arrived in the area.
The park's southern entrance is a few hundred metres north of Mondzo at, a one-day hike from Lukla. A visitor centre is located at the top of a hill in Namche Bazaar.