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The Brahmaputra is a trans-boundary river which flows through Tibet ( China ), Northeastern India, and Bangladesh. It is known as Brahmaputra or Luit in Assamese, Yarlung Tsangpo in Tibetan, the Siang/Dihang River in Arunachali, and Jamuna River in Bengali. It is the 9th largest river in the world by discharge, and the 15th longest .
May 4, 2024 · Explore the Brahmaputra River's course, tributaries, and impact on landscapes and livelihoods. Learn about its journey from Tibet to Bangladesh.
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5 days ago · After flowing past Chilmari, Bangladesh, it is joined on its right bank by the Tista River and then follows a 150-mile (240-km) course due south as the Jamuna River. (South of Gaibanda, the Old Brahmaputra leaves the left bank of the main stream and flows past Jamalpur and Mymensingh to join the Meghna River at Bhairab Bazar.)
It runs for a length of 2880 km and its river system drains parts of China, Bhutan, India and Bangladesh. Considerable variations in width, gradient, discharge and channel pattern occur throughout its course. The system is described here by dividing the course into ten unequal reaches.
- J. N. Sarma
- 2004
Jan 3, 2018 · The Brahmaputra is known by different names along its course. Figure 1 shows the elevation map of the Brahmaputra basin along with its tributaries. The Brahmaputra originates in the snow-covered Kailash Mountain (the Jimayangzhong Glacier) in Trans-Himalaya, flows eastward on a very gentle slope (~0.001) for ~1200 km along the Indus-Tsangpo Suture in Tibet (Fig. 2) and known as theYarlung ...
- Sunil Kumar Singh
- sunil@prl.res.in
- 2018
Oct 5, 2021 · The largest and most populous delta system in the world is the Ganges–Brahmaputra–Meghna (GBM) delta, located in Bangladesh and West Bengal, India (Fig. 1).
Isabel Hilton, thethirdpole.net editor. Brahmaputra: Towards unity Introduction. 5. Today, though, as the essays in this volume explore, this great river is under threat: climate change will alter its flow over the long-term, as glaciers and monsoon patterns and ground water reserves react to rising temperatures and changing patterns of use.
