Subject GS Paper 3: Environment
Context: A first-of-its-kind study by IIT Gandhinagar has found that precipitation in the catchments of the eastern rivers (Ravi, Beas, and Sutlej) declined by nearly 20% between 1951 and 2024, providing scientific evidence that climate change has significantly altered water availability in the Indus River Basin.
- The findings strengthen India’s case for revisiting the Indus Waters Treaty (IWT), 1960.
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Key Findings of the Study
- Declining Rainfall in Eastern Rivers
- 20% decline in precipitation in the Ravi, Beas, and Sutlej catchments (1951–2024).
- These rivers are allocated exclusively to India under the Indus Waters Treaty.
- Stable Rainfall in Western Rivers
- Indus, Jhelum, and Chenab recorded only a 6% decline, which is statistically insignificant.
- Water availability in Pakistan’s allocated rivers has remained relatively stable.
- Groundwater Depletion
- Significant depletion of groundwater observed in the Ravi and Sutlej sub-basins.
- Western river basins showed relatively healthier groundwater due to:
- Lower agricultural pressure.
- Lower population density.
- Greater recharge from snowfall and precipitation.
- Declining Reservoir Inflows
- Major Indian reservoirs witnessed a substantial fall in annual inflows:
- Pong Dam: Nearly 34% decline (1951–2020).
- Bhakra and Thein reservoirs also recorded declining inflows.
- In contrast, Pakistan’s Mangla and Tarbela reservoirs showed only marginal declines.
Why is Study Important?
- Provides the first scientific, data-based evidence that climate change has altered hydrological conditions in the Indus Basin.
- Supports India’s argument that the hydrological assumptions underlying the Indus Waters Treaty (1960) have fundamentally changed.
- Highlights that water availability is no longer consistent with the conditions prevailing when the treaty was signed.
India’s Position on the Indus Waters Treaty
India has argued that the Treaty requires review and modification because of:
- Climate change altering river flows.
- Population growth increases water demand.
- Need for clean energy expansion (hydropower).
- Changing developmental requirements.
- Increased variability in rainfall and water availability.
Following the Pahalgam terrorist attack (2025), India declared the Treaty to be “in abeyance”, while reiterating that it would remain so until Pakistan credibly and irrevocably ends support for cross-border terrorism.
Implications for India
- Water Security: Reduced water availability in eastern rivers could affect:
- Irrigation.
- Drinking water supply.
- Agricultural productivity.
- Hydropower: Lower reservoir inflows may reduce hydropower generation in northern India.
- Climate Adaptation: Highlights the need for climate-resilient river basin management and improved groundwater governance.
- Transboundary Water Governance: Demonstrates that water-sharing agreements should incorporate climate variability and adaptive management.
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Indus River System
| River |
Origin |
Key Features |
Joins |
| Indus |
Near Lake Manasarovar, Tibet (close to Mount Kailash) |
Enters India at Demchok (Ladakh); flows through Ladakh into Pakistan; empties into the Arabian Sea |
Arabian Sea |
| Jhelum |
Verinag Spring, Kashmir |
Flows through Wular Lake and Srinagar; known as Vitasta in ancient texts |
Chenab (in Pakistan) |
| Chenab |
Confluence of Chandra and Bhaga rivers at Tandi (Himachal Pradesh) |
Longest tributary of the Indus; major hydropower projects (Salal, Baglihar, Ratle) |
Indus (via Panjnad in Pakistan) |
| Ravi |
Near Rohtang Pass, Himachal Pradesh |
Forms part of the India–Pakistan border; ancient name Iravati |
Chenab (in Pakistan) |
| Beas |
Beas Kund, near Rohtang Pass, Himachal Pradesh |
Entirely flows within India; ancient name Vipasha |
Sutlej at Harike, Punjab |
| Sutlej |
Lake Rakshastal, Tibet (near Mount Kailash) |
Longest of the five Punjab rivers; enters India through Shipki La; Bhakra-Nangal Dam |
Chenab (via Panjnad in Pakistan) |