Context: The Chief Minister of Assam addressed concerns surrounding the Brahmaputra River, emphasising that 65-70% of the Brahmaputra’s flow is generated within India, reassuring the public about India’s water sovereignty.
Relevance of the Topic: Prelims: Key facts about Brahmaputra River System; Key Hydropower Projects.
Hydrology of Brahmaputra River
- Brahmaputra originates as Yarlung Tsangpo in Kailash range near Mansarovar lake in Tibet. It traverses more than 1,000 km eastward, before forming a horseshoe bend around the Namcha Barwa peak, and enters near Gelling in Arunachal Pradesh as the Siang (or Dihang).
- Brahmaputra is primarily a rain-fed river system, with only approximately 30-35% of its flow coming from China, mostly through glacial melt and scanty rainfall that happens in the Tibetan region.
- The majority of the river’s water (about 65-70%) arises within India itself due to the monsoon rains that pour over the Northeast’s hilly terrains and the numerous tributaries feeding the river.
- The river is called Siang in Arunachal, is joined by many tributaries in Assam as it flows down the plains before entering Bangladesh, where it is called Jamuna.
| Left/ South bank Tributaries of Brahmaputra | Right/ North bank Tributaries of Brahmaputra |
| Dihang | Kameng |
| Dibang | Manas |
| Lohit | Subansari |
| Noa Dehing | Dhansiri (North) |
| Burhi Dehing | Sankosh |
| Kopilli | Ronganadi |
| Dhansiri (South) | |
| Kolong |

Hydro-statistics and Regional data
- Brahmaputra’s flow at key points exemplifies India’s water independence. At the Indo-China border, near the Tuting region in Arunachal Pradesh, the flow rate is around 2,000-3,000 cubic metres per second.
- During the monsoon season, as the river enters Assam’s plains, the flow swells to an impressive 15,000-20,000 cubic metres per second.
- These figures underscore that the river’s strength and volume are predominantly sustained within India’s climatic and geographical domain. Thus, India does not depend on upstream water flow from China to sustain its water needs.
As the region faces severe flooding due to monsoons, India must emphasise resilience and infrastructure over fears of upstream interference.
Impact of Hypothetical reduction of water by China
- Even a hypothetical reduction in Chinese water contribution would have a minimal impact on India’s water security or be potentially beneficial. Reduced flow could mitigate the devastating floods that annually ravage Assam and the northeastern region.
This point also highlights that India’s water system is resilient and primarily driven by monsoon rains and local tributaries.
China’s planned interventions on Brahmaputra
Most of the Chinese infrastructure interventions are hydropower projects with minimal storage, and are located far upstream of Arunachal Pradesh, with no significant impact in Arunachal or Assam.
- Medog (or Motuo) Hydropower Project: A major concern is the planned massive dam in Medog County near the ‘Great Bend’ where the river makes a U-turn and plunges into a canyon before entering Arunachal Pradesh. The planned 60,000-MW Medog project will be the world’s largest hydropower facility, with a generation capacity three times that of the Three Gorges Dam on the Yangtze, currently the world’s largest hydropower station.
- South-North Water Diversion (SNWD) project: Concerns have also been raised over China’s massive, multi-decade South-North Water Diversion (SNWD) project, the Western Route of which apparently involves diverting water from the Yarlung Tsangpo (and other rivers) to the country’s dry northern regions.
As a mitigation strategy, India could plan storage on rivers of the Brahmaputra system to absorb the variations in flows (periods of flooding and reduced flows). E.g., The Upper Siang Project will not only generate power, its storage can also serve as a buffer against variations in flows.
India’s interventions to utilise water potential of Brahmaputra:
Brahmaputra and its tributaries carry more than 30% of India’s total water resources potential, and 41% of the total hydropower potential, as per estimates in the CWC-ISRO Brahmaputra Basin Atlas.
- The National Water Development Authorityhas proposed two links to connect the Brahmaputra and its tributaries to the Ganga basin with the aim of transferring surplus water to water-scarce regions. These are:
- Manas-Sankosh-Teesta-Ganga Link, joining the Manas, a tributary of the Brahmaputra, to the Ganga via the Sankosh and Teesta
- Jogighopa-Teesta-Farakka Link, joining the Brahmaputra at the planned Jogighopa Barrage to the Ganga at the Farakka Barrage.
- However, utilisation of hydropower in Arunachal Pradesh has been slow due to difficulties of land acquisition and concern over the submergence of forest lands, etc.
Environmental Risks:
- Risks of flooding may arise from intentional or unintentional operation of reservoirs in Tibet, as well as unforeseen events such as dam failure, landslides, or earthquakes.
- Upstream interventions have the potential to affect the river morphology, with consequences for riverine flora and fauna.
Key Facts:
- Tibetan Plateau is a region of scant rainfall of the order of 300 mm annually.
- The southern part of the Brahmaputra river basin in India receives 2,371 mm of rain on average every year, and very few places receive less than 1,200 mm.
India should work to actively seek detailed hydrological and project-related data to continuously assess the downstream impact of Chinese infrastructure interventions and develop comprehensive data sharing protocols with China for advance warning and disaster preparedness.






