Koshi (कोसी, कोशी) |
Sapt Koshi, सप्तकोसी |
River |
|
Countries |
Nepal, India |
State |
Bihar |
|
Cities |
Biratnagar, Purnia, Katihar |
|
|
Source |
Confluence of the Sun Kosi, Arun and Tamur to form Sapta Kosi |
- location |
Tribenighat, Nepal |
- coordinates |
26°54′47″N 87°09′25″E / 26.91306°N 87.15694°E / 26.91306; 87.15694 |
Mouth |
Ganges |
- location |
near Kursela, Bihar, India |
- coordinates |
25°24′43″N 87°15′32″E / 25.41194°N 87.25889°E / 25.41194; 87.25889 |
|
Length |
729 km (453 mi) |
Basin |
69,300 km2 (26,757 sq mi) |
Discharge |
for Ganges River |
- average |
2,166 m3/s (76,492 cu ft/s) [1] |
|
|
The Kosi River (Hindi: कोसी नदी) or Koshi (Nepali: कोशी नदी)—also Saptakoshi (Nepali: सप्तकोशी) for its seven Himalayan tributaries—is a trans-boundary river flowing through Nepal and India. Some of the rivers of the Koshi system, such as the Arun, the Sun Kosi and the Bhote Koshi, originate in the Tibet Autonomous Region of China. It is one of the largest tributaries of the Ganges.
Along with its tributaries, the river drains 29,400 km2 (11,400 sq mi) in China (mainly the upper Arun basin north of the Mount Everest region), 30,700 km2 (11,900 sq mi) in Nepal (the eastern third of the country), and 9,200 km2 (3,600 sq mi) in India.
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 48 km (30 mi) north of the Indo-Nepal border. Below the Siwaliks the river has built up a megafan some 15,000 km2 (5,800 sq mi) in extent, breaking into more than twelve distinct channels with shifting courses due to flooding.[2][3] Kamlā, Bāghmati (Kareh) and Budhi Gandak are major tributaries of Koshi in India, besides minor tributaries like Bhutahi Balān.[4][5]
Over the last 250 years, the Kosi River has shifted its course over 120 km (75 mi) from east to west.[6] Its unstable nature has been attributed to the heavy silt it carries during the monsoon season. Flooding in India has extreme effects, and the country is second in the world after Bangladesh in deaths due to flooding, accounting for one fifth of global flooding deaths. The Kosi River (The Sorrow of Bihar) is one of two major tributaries, the other river being the Gandak, draining the plains of north Bihar, the most flood-prone area of India[7] Fishing is an important enterprise on the river but the fishing resources are being depleted and the younger fishermen are leaving for other areas of work.[8]
The Koshi was also called Kausika in Rigveda, in Nepal and Bihar in northern India is a major tributary of the 'Ganges' one major tributary of the Koshi is the Arun, a major part 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' '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 Koshi. Viśvāmitra was descendant of sage Kusika. Viśvāmitra is credited with writing many well known Vedic Hymns on the Banks of the Kosi were he had is 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 (3.62.10).
The mantra is named for its vedic gāyatrī metre.[1] As the verse can be interpreted to invoke the deva Savitr, it is often called Sāvitrī.[2] Its recitation is traditionally preceded by oṃ and the formula bhūr bhuvaḥ svaḥ, known as the mahāvyāhṛti ("great utterance"). The Gayatri Mantra is repeated and cited very widely in vedic literature,[3] and praised in several well-known classical Hindu texts such as Manusmṛti,[4] Harivamsa,[5] and the Bhagavad Gita.
The Koshi (Kosi in Sanskrit) is associated with many ancient spiritual stories. Kosi is mentioned in the Bal Kand section of Valmiki Ramayana as the Kausiki who is the form assumed by Satyavati after her death. Satyavati was the elder sister of Viswamitra, descendants of Kushak dynasty. In the Markendeya Purana, the Kosi is described as the primal force. Do to the violent nature of the Kosi during monsoon season, legend says that Parvata, the wife of Shiva, after defeating the demon Durg, became known as the warrior goddess Durga who transformed into Kaushiki. In Ramayana, the river Ganges is depicted as her elder sister.
According to Mahabharata epic, the God of death took the form of a woman and resides on the banks of the river to keep the growth of human population under check. Kosi resonates with the folklore of Mithila region. The most important depictions of Kosi folklore are Kosi as a virgin absolutely care free and full of energy; As a frustrated wife of old hermit Richeek wandering in Himalayas. Kosi is also invoked as the mother - 'Kosi Ma'. These images capture the contradiction that is inherent in the Kosi 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', and parts of adjoining Nepal. 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.
From Katmandu, there is a road for some distance followed by trekking paths to Mt Everest, which crosses four major tributaries of the Koshi. Namche Bazar near Tibet border in Nepal (near southern base camp of Mt Everest) is the major tourist centre in the mountainous part of the Koshi belt. Birātnagar in Nepal, and Purnia and Katihār in India are major cities on the Koshi Plains. Kamlā, Bāghmati (Kareh) and Budhi Gandak are major tributaries of Koshi in India, besides minor tributaries like Bhutahi Balān.
In Nepal, the Koshi basin is bordered on the west and the south-west by the basins of the Gandaki and the Burhi Gandak. The Bagmati river (draining Kathmandu Valley) sub-basin forms the south-western portion of the overall Koshi basin. The Kanchenjunga Himalayas are its eastern watershed, with the Singalila Ridge forming the border with the Teesta basin. Its basin contains 6 of the 14 mountains in the world higher than 8,000m (including 5 of the 6 highest). The 6 peaks are Mount Everest, Kangchenjunga, Lhotse, Makalu, Cho Oyu and Shishapangma. Mount Everest is the highest point of the Koshi basin. The Koshi has seven major tributaries: Sun Kosi (Nepali: सुनकोशी), Tamakoshi (तामाकोशी) or Tamba Koshi, Dudh Kosi (दुधकोशी), Indravati (इन्द्रावती), Likhu (लिखू), Arun (अरुण) and Tamur (तमोर).
The Dudh Kosi joins the Sun Kosi at the Nepalese village of Harkapur. At Triveni the Sunkoshi from the west is joined by the Arun from the north (the Dudhkoshi and Arun encircle Mount Everest), then the Tamar from the east. The combined river becomes the Saptakoshi (सप्तकोशी), literally "Seven Koshis". The Saptakoshi crosses the Lesser Himalaya or Mahabharat Range in a deep gorge some 10 km (6.2 mi) long. At Barāhkṣetra in Nepal it emerges from the mountains and becomes the Koshi. After flowing another 58 km (36 mi) it crosses into Bihar, India, near Bhimnagar and after another 260 km (160 mi) joins the Ganges near Kursela. The river has a total length of 729 km (453 mi).
The Kosi alluvial fan is one of the largest in the world, and extends from Barāhkṣetra across Nepalese territory then northeast Bihar and eastern Mithila to the Ganges, 180 km (110 mi) long and 150 km (93 mi) wide. It shows evidence of lateral channel shifting exceeding 120 km (75 mi) 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.[9] The alluvial cone and its adjoining area have been studied by remote sensing techniques. These data have been combined with geological and geophysical information to infer causes responsible for the lateral shifts.
There are two national parks in the Koshi river basin:
Sagarmatha National Park is located in eastern Nepal, including parts of the Himalayas and the southern half of Mount Everest. The park, which is also included as a UNESCO world heritage site, was created on 19 July 1976. Sagarmatha in Sanskrit means "Forehead of Universe" (Sagar: Sky or Heavens; Matha: Forehead) and is the modern Nepali name for Mount Everest. The park covers an area of 1,148 km2 (443 sq mi) and ranges in elevation from its lowest point of 2,845 m (9,334 ft) at Jorsalle to 8,848 m (29,029 ft) at the summit of Mount Everest (highest peak in the world).[10] Other peaks above 6,000 m (20,000 ft) are Lhotse, Cho-Oyu, Thamserku, Nuptse, Amadablam, and Pumori. The upper watershed of the Dudh Kosi river basin system lies in the park. The types of plants and animals that are found in the park depend on the altitude.
The forests provide habitat to at least 118 species of birds, including Himalayan Monal, Blood Pheasant, Red-billed, and Alpine Chough. Sagarmatha National Park is also home to a number of rare species, including musk deer, wild yak, snow leopard, Asian Black Bear and red panda. Moreover, many other animals such as Himalayan thars, deer, langur monkeys, hares, mountain foxes, martens, and Himalayan wolves are found in the park.
In the lower forested zone, birch, juniper, blue pines, firs, bamboo and rhododendron grow. Above this zone, all vegetation is dwarf plants or shrubs. As the altitude increases, plant life is restricted to lichens and mosses. Plants cease to grow at about 5,750 m (18,860 ft), in the permanent snowline in the Himalayas.
The park's visitor centre is located at the top of a hill in Namche Bazaar, also where a company of the Nepal Royal Army is stationed to protect the park. The park's southern entrance is a few hundred metres north of Mondzo at 2 835 m (9,300 ft), a one-day hike from Lukla.
The presence of the Sherpas, with their unique culture, adds further interest to this park.[11] UNESCO listed the park as a World Heritage Site in 1979 for its unique natural, cultural and landscape characteristics.[10]
Koshi Tappu Wildlife Reserve is a wetland situated in the flood plains of the Sapta-Koshi River in Nepal's eastern Terai. Gazette-notified as a wild life reserve in 1976, it covers a reserve area of 175 km2 (68 sq mi) and is one of the Outstanding Important Bird Areas in the Indo-Gangetic grasslands. The park has large population of Swamp Francolin, breeding Bristled Grassbird, records of Hodgson's Bushchat and Finn's Weaver.[12] The Koshi river forms the major landmark of the reserve and is home to 80 fish species, around 441 species of birds, 30 shore birds, 114 water birds, 20 ducks and 2 ibises. The endangered Bengal Florican is also found here. The Koshi Barrage is an extremely important resting-place for migratory birds (87 nos winter visitors). In view of its rich biodiversity it was declared a Ramsar site of international significance in 1987.[13] The endangered Gharial crocodile and Gangetic dolphin locally known as sons in Bihar and a further endangered species (freshwater dolphin) have been recorded in the river.
The last surviving population of wild buffalo or arna in Nepal is found in the reserve (number at present is estimated to be 150). The reserve is a habitat of 20 other animal species such as hog deer, spotted deer, wild boar, blue bull and rock python.
The vegetation mainly includes tall khar-pater grasslands with a few patches of khair-sissoo scrub forest and deciduous mixed riverine forest.
During the monsoon, the reserve is flooded with depths ranging from 10 to 300 cm (3.9 to 120 in). Birdwatching along the eastern embankment at dusk and dawn is one of the most exciting tourist attractions in the reserve.[14] Gangetic River Dolphin, locally known as sons in Bihar, is an endangered species (freshwater dolphin).[15]
The Kosi is known as the "Sorrow of Bihar" as it flows from Nepal to India,[6] as it has caused widespread human suffering in the past through flooding and very frequent changes in course [2] [3] [4].
The Koshi has an average water flow (discharge) of 2,166 cubic metres per second (76,500 cu ft/s).[1] During floods, it increases to as much as 18 times the average. The greatest recorded flood was 24,200 m3/s (850,000 cu ft/s) on 24 August 1954. The Kosi Barrage has been designed for a peak flood of 27,014 m3/s (954,000 cu ft/s)(2).
Extensive soil erosion and landslides in its upper catchment have resulted in the silt yield of the Kosi of about 19 m³/ha/year (10 cu yd/acre/yr), one of the highest in the world. (2). Of major tributaries, the Arun with its origins in Tibet brings the greatest amount of coarse silt in proportion to its total sediment load. The river is able to transport its heavy sediment load 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, even 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 to be 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. Instead of a single well-defined channel, the river has numerous interlacing channels that shift laterally over the fan from time to time. Without sufficient 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, flowing down the slight slope of the alluvial fan at one metre per second.
The Kosi'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. It contributes disproportionately to India having more deaths in floods than any other country except Bangladesh.
-
The Kosi before it flooded in August 2008
-
The Kosi during the August 2008 flood
On 18 August 2008, the Kosi river picked up an old channel it had abandoned over 100 years ago previously near the border with Nepal and India. Approximately 2.7 million people were reported affected as the river broke its embankment at Kusaha in Nepal, thus submerging several districts of Nepal and India. 95% of total flow of the Koshi was reported flowing through the new course.[16][17] The worst affected districts included Supaul, Araria, Saharsa, Madhepura, Purnia, Katihar, parts of Khagaria and northern parts of Bhagalpur, as well as adjoing 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.[16] The magnitude of deaths or destruction have been hard to estimate, as the affected areas are inaccessible. 150 people were reported washed away in a single incident (Dainik Hindustan, Darbhanga edition). Another news item stated that 42 people had died in the flood in Bihar.[18]
The Government of Bihar has convened a technical committee, headed by a retired engineer-in-chief of the water resource department to supervise the restoration work and closure of the breach in the East Kosi afflux embankment.[18] Indian authorities were working to prevent further widening of the breach, and channels were to be dug to direct the water back to the main river bed.[19]
The fury of the Koshi river left at least 2.5 million people marooned in eight districts of Bihar and inundated 650 km². The prime Minister of India declared it a national calamity. The Indian Army, National Disaster Response Force (NDRF) and non-government organizations were operating the biggest flood rescue operation in India in more than 50 years.[20] It is reported as the worst flood in the area in 50 years.[21]
In the Himalayas, glaciers are melting and retreating, which results in formation of lakes insecurely dammed by ice or moraines. These dams are at risk of breaking, causing a Glacial Lake Outburst Flood (GLOF) with flows as great as 10,000 cubic metres a second. Such floods are likely to destroy communication systems and various infrastructures like bridges roads, hydropower projects, foot trails, villages, fields and terraces, irrigation canals, and could cost hundreds or even thousands of lives. Such floods also transport huge amounts of sediment.
In the past two decades GLOF has become a topic of intense discussion within the development community in Nepal. Studies of the glaciers and glacier lakes were carried out in 1988 by a joint Sino-Nepalese team. In the Arun-Koshi river basin, there are 737 glaciers in Tibet and 229 glacier lakes, out of which 24 glacier lakes are potentially dangerous. Similarly, there are 45 glacier lakes in the Sun-Koshi basin, out of which 10 are potentially dangerous.
The Dig Tsho GLOF on 4 August 1985, completely destroyed the nearly completed Namche hydropower plant and also all the bridges, trails, cultivation fields, houses and livestock along its path to the confluence of the Dudh-Koshi and the Sun-Koshi rivers at a distance of 90 km (56 mi) from the Dig Tsho glacier. 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.
According to a Sino-Nepalese study, since the 1940s, there have been at least 10 cases of glacier lake outbursts within the basins investigated. Among them there have been five bursts in three glacier lakes of the Arun River Basin, and four in three glacier lakes of the Sun Koshi River Basin.
After India attained independence in 1947, the India has pushed forward with technological development. The National Flood Control Policy in 1954 (following the disastrous floods of 1954 in a large part of the Koshi river basin) stated that floods could be controlled through a series of flood protection works like dams, embankments and river training works. Immediately after independence, policy planners sought a solution to the recurring flood menace faced by people of North Bihar from the Kosi and other rivers flowing from Nepal to India. The Kosi project was thus conceptualized (based on investigations between 1946 to 1955), in three continuous interlinked stages – the first was a barrage to anchor this wayward river that had migrated about 120 km (75 mi) 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 so as to jacket the river within the defined channel. The third part envisaged a high multipurpose dam within Nepal at Barakshetra to provide substantial flood cushion along with large irrigation and power benefits to both countries. This was followed up by signing of the Kosi Agreement between Nepal and India on 25 April 1954 and which was revised on 19 December 1966 to address the concerns of Nepal. Further letters of Exchange to the Agreement between the two countries provided for additional schemes for providing benefits of irrigation. While the first two parts of the concept plan have been implemented at the cost of the Government of India, the third part, namely, the Koshi High dam, the kingpin of the whole concept, for various political reasons precluded any action for several years but has since been revived under a fresh agreement, in a modified form for further investigations and studies(1,2,3,4 & 5).
Kosi Barrage, also called Bhimnagar Barrage after the name of the place where it was built between the years 1959 and 1963, straddles the Indo-Nepal border. It is an irrigation, flood control and hydropower generation project on the Kosi 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 61,788 km2 (23,856 sq mi) in Nepal at the Barrage site. The highest peaks – the Mount Everest and the Mount Kanchenjunga — lie in its catchment. About 10% of this catchment is snow-fed. The Eastern Canal and the Western Canal taking off from the barrage have been designed for a discharge capacity of 455 cubic metres per second (16,100 cu ft/s) to irrigate 6,125 square kilometres (1,514,000 acres) and 210 cubic metres per second (7,400 cu ft/s) to irrigate 3,566.1 square kilometres (881,200 acres) respectively. A hydropower plant has been built on the Eastern Canal, at a canal drop (3.6 km (2.2 mi) from the Koshi Barrage), to generate 20 MW. The Western Kosi Canal provides irrigation to 250 square kilometres (62,000 acres) 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 Kosi debouches into the plains, has been built to irrigate a gross area of 860 km² in Nepal. The project has been renovated with IDA assistance after Nepal took over the project in 1976.
The Kosi barrage with earth dams across river, 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 246 km (153 mi) has been constructed to check the westward movement of the river. The embankments have been kept far apart, about 12 to 16 km (9.9 mi), to serve as a silt trap
The governments of India and Nepal have 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 Kosi Storage-cum-Diversion Scheme to meet the objectives of both the countries for development of hydropower generation, irrigation, flood control and management and navigation.
Envisaged are a 269-metre (883 ft) high concrete or rock filled dam on the Sapta Koshi River with a dam to the underground power house, with an installed capacity of 3000 MW at 50% load factor, a barrage on Sapta Koshi about 8 km (5.0 mi) downstream of Sapta Koshi High Dam to re-regulate the water being released from the Sapta Koshi dam with two canals, Eastern Chhatra Canal and Western Chhatra Canal, off-taking from the either bank from 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 off-taking from the Eastern Chatra Canal is proposed for conveying the water required for irrigation at existing Koshi barrage at Hanuman Nagar and also the water which may be required downstream of Hanuman Nagar Barrage for the purpose of 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 also proposed on power canal.
Necessary cushion in storage capacity of Sapta Koshi High Dam would be provided to moderate the flood downstream of dam.
Chatra Canal System would provide irrigation to large areas in Nepal and India (particularly in Bihar).
A Joint Project Office (JPO) has been set up in Nepal for investigation of the project.
Nepal has a total estimated potential of 83,290 MW out of which economically exploitable potential is 42,140 MW. The Koshi river basin contributes 22,350 MW of this potential.(360 MW from small schemes and 1875 MW from major schemes) and the economically exploitable potential is assessd as 10,860 MW (includes the Sapta Koshi Multipurpose Project [3300MW] mentioned above).[22]
River rafting, also known as White Water Rafting, is an adventure sport that challenges one’s ability to row against the current of rivers. This is usually done on whitewater or different degrees of rough water, to thrill and excite the passengers riding on an inflatable rubber raft. It became popular as a sport during the mid 1970s and is now the third most popular adventure sport in Nepal after mountaineering and trekking. The Sun Koshi river (The Golden River) presents the longest river trip in Nepal, traversing 270 km (170 mi) and meandering its way through the picturesque Mahabharata range of mountains. The river rafting trip in the Sun Koshi is listed as one of the world’s top ten classic river journeys. Other rivers where this adventure sport is a popular tourist attraction in Nepal are the Kali Gandaki, the Trisuli, the Bhote Koshi, the Marsyangdi and the Karnali.[23] and [24]
A classic multi-day River trip (9 days) with around 40 rapids of grade 2-5 (Rivers are graded on a scale from one to six based on rapids and difficulties in rafting through the river) is recommended for advanced Rafters and Kayakers.[25]
The Koshi and other rivers draining the Himalayas have populations of Mahseer which are esteemed as gamefish and known as Indian Salmon. Mahseer can weigh up to 50 kg. and are said to put up a greater battle than any other type of fish of equivalent weight. They will take tied streamer flies as well as bait.
- ^ a b Jain, Sharad K.; Agarwal, Pushpendra K.; Singh, Vijay P. (2007). Hydrology and water resources of India. Springer. p. 341. ISBN 978-1-4020-5179-1. http://books.google.com/books?id=ZKs1gBhJSWIC&pg=PA341. Retrieved 26 April 2011.
- ^ Rao, K.L. (1975) India's Water Wealth. Orient Longman Ltd., Hyderabad, New Delhi.
- ^ Vargehese, B.G. (1993) "Waters of Hope". New Delhi
- ^ "Koshi River". Encyclopædia Britannica. Encyclopædia Britannica Online. Encyclopædia Britannica Inc.. 2011. http://www.britannica.com/eb/article-9046108/Koshi-River. Retrieved 2007-08-24.
- ^ "Koshi River, Bihar, India". The Geospacial Research Portal - Natural Hazard Management. http://ponce.sdsu.edu/kosi_river_india.html. Retrieved 2007-08-24.
- ^ a b "The Sorrow Of Bihar: Koshi River". Nepalnews.com. http://www.nepalnews.com.np/contents/englishweekly/spotlight/2004/jun/jun04/opinion.htm. Retrieved 2007-08-24. [dead link]
- ^ Bapalu, G. V., Sinha, R., GIS in Flood Hazard Mapping: a case study of Koshi River Basin, India, Geospatial Media and Communications Pvt. Ltd., http://www.geospatialworld.net/index.php?view=article&catid=149%3Anatural-hazard-management-flood-cyclones&id=15981%3Agis-in-flood-hazard-mapping-a-case-study-of-kosi-river-basin-india&format=pdf&option=com_content&Itemid=41, retrieved 2011-11-25
- ^ "The current status of capture fishery in the upper Sunkoshi River. (by R. Ranjit)". Inland Aquaculture and Fisheries Section, IAFS, Central Fisheries Building, Balaju, Kathmandu, Nepal. http://www.fao.org/docrep/005/y3994e/y3994e0s.htm.
- ^ Abstract Agarwal, R. P. and Bhoj R. (1992) "Evolution of Koshi river fan, India: structural implications and geomorphic significance" International journal of remote sensing 13(10): pp. 1891-1901;
- ^ a b Sagarmatha National park - Background
- ^ Sagarmatha National Park - UNESCO World Heritage Centre
- ^ http://www.birdlife.org/action/science/species/asia_strategy/pdf_downloads/grasslandsGO2.pdf.
- ^ http://www.south-asia.com/dnpwc/other-national-parks/koshi-tappu.htm and Gangetic River Dolphin (Platanista gangetica)- Rapidly diminishing
- ^ Koshi Tappu Wildlife Reserve
- ^ Gangetic River Dolphin (Platanista gangetica)- Rapidly diminishing [1]
- ^ a b "Bihar flood 'catastrophe'; CM seeks Govt's help". CNN IBN. 2008-08-26. http://www.ibnlive.com/news/bihar-flood-catastrophe-cm-seeks-govts-help/72143-3.html?from=rssfeed. Retrieved 2008-08-26.
- ^ "Flood devastation in Bihar state". BBC. 25 August 2008. http://news.bbc.co.uk/2/hi/south_asia/7580587.stm. Retrieved 2008-08-26.
- ^ a b "Koshi wreaks havoc in Bihar, claims 42 lives". Press Trust of India (NDTV). 26 August 2008,. http://www.ndtv.com/convergence/ndtv/story.aspx?id=NEWEN20080062979&ch=8/26/2008%2012:36:00%20PM. Retrieved 2008-08-26.
- ^ "Bihar floods: 47 die; thousands marooned". IST,AGENCIES (Times of India). 26 August 2008. http://timesofindia.indiatimes.com/India/Bihar_floods_47_die_thousands_hit/articleshow/3405430.cms. Retrieved 2008-08-26.
- ^ http://timesofindia.indiatimes.com/Editorial/After_the_Deluge/articleshow/3429471.cmsAfter the Deluge
- ^ nytimes.com, Floods in India May Displace Millions
- ^ Nepalnews.com Mercantile Connumications Pvt. Ltd
- ^ http://www.infohub.com/vacation_packages/11199.html.
- ^ Rafting Activity in Nepal from nepalvista.com
- ^ Sunkoshi River Rafting, Nepal Sunkoshi River, Sunkoshi River, Sunkoshi River Rafting in Nepal, Nepal Rafting Agents, Rafting Association in Nepal, Nepal Rafting Association, Rafting in Nepal, Nepal Raft, Nepal Raft Agents, Raft Agents in Nepal, Nepal Rafting Agencies,Nepal Rafting, Adventure Rafting Nepal, Nepal Adventure Rafting, Seti River Rafting, Trishuli River Rafting, Kali Gandaki Rafting, Sun Koshi Rafting, Karnali, Bheri, Tamur and Arun Rivers, White Water Rafting in Nepal, Marshangdi River Rafting
- Floods, Flood plains and Environmental Myths – State of Art of India’s Environment – A Citizens’ Report, Centre for Science and Environment, 807, Vishal Bhavavn, 95, Nehru Place, New Delhi - 110019.
- A Framework for Sustainable Development of the Ganges- Brahmaputra- Meghna (GBM Region), Proceedings of Conference held in Dhaka, 4–5 December 1999–Nepal Water Vision in the GBM Regional Framework, Institute for Integrated Studies, Kathmandu).
- Water Conflicts in South Asia, Managing Water Resources Disputes Within and Between Countries of the Region (2004), Published by GEE-21Honolulu Hi 96825-0517,USA.
- Barrages in India (1981), Publication number 148, Central Board of Irrigation and Power, Malcha Marg, Chanakyapuri, New Delhi.
- Design and Construction of selected Barrages in India (1981), Publication number 149, Central Board of Irrigation and Power, Malcha Marg, Chanakyapuri, New Delhi.
|
|
Inland |
|
|
Coastal |
|
|
Categories |
|
|
|
|
Rivers |
Mahananda basin
|
|
|
Sapta Koshi basin
|
|
|
Bagmati basin
|
|
|
Narayani basin
|
|
|
Karnali basin
|
|
|
|
Lakes |
|
|
Glaciers |
|
|
Icefalls |
|
|
Related topics |
|
|
|
|
Rivers |
|
|
Waterfalls |
|
|
Dams, barrages |
|
|
Bridges |
|
|
Related topics |
|
|
Hydrography of surrounding areas |
|
|
|
|
Rivers |
|
|
Dams, barrages, bridges |
|
|
Geographical features |
|
|
Important localities |
|
|
Floods |
|
|
Riparian districts/ areas |
|
|
Languages/ people |
|
|
Transport |
|
|
Other basins |
|
|