GS Paper 1 10 marks · 150w 9 min Medium
How will the melting of Himalayan glaciers have a far-reaching impact on the water resources of India?
Subtopic: Geography · Himalayan cryosphere and India's water resources
How to structure your answer
Introduction → Establish glacier–river dependence (Third Pole, ICIMOD warnings) → Short-term impacts: enhanced melt, floods, GLOFs → Long-term impacts: peak water, lean-season scarcity, irrigation and hydropower stress → Wider effects: springs, groundwater, deltas → Conclusion with adaptation measures
Detailed model answer
189 words · target 150 words · 9 min
Himalayan glaciers — the 'Third Pole' — feed the Indus, Ganga and Brahmaputra systems on which nearly half of India's population depends. ICIMOD's Hindu Kush Himalaya assessments warn that glaciers could lose a third of their ice by 2100 even at 1.5°C warming, and far more under high emissions.
Far-reaching impacts on water resources
- Deceptive plenty first: accelerated melt initially raises river flows, swells glacial lakes and triggers outburst floods — Kedarnath (2013), Chamoli (2021) and the South Lhonak–Teesta disaster (2023).
- Scarcity later: after 'peak water', dry-season discharge declines; the Indus, most dependent on meltwater, faces the sharpest stress, threatening Punjab's irrigation economy.
- Agriculture: shrinking lean-season flows hit rabi irrigation across the Indo-Gangetic plain and deepen dependence on already-stressed groundwater.
- Hydropower and dams: erratic discharge and heavy sediment-debris loads endanger projects — Tapovan-Vishnugad was wrecked in 2021 and Teesta-III washed away in 2023.
- Drinking water: Himalayan towns face shortages (Shimla, 2018), and NITI Aayog notes nearly half of Himalayan springs are drying.
- Deltas: altered freshwater-sediment flux worsens salinity intrusion in the Sundarbans.
India needs sustained cryosphere monitoring, GLOF early-warning systems, climate-proofed hydropower siting, basin-level cooperation with neighbours and demand-side water efficiency under the National Mission for Sustaining the Himalayan Ecosystem.
What an examiner expects to see
- Himalaya as Asia's water tower: meltwater sustains Indus, Ganga and Brahmaputra base flows; Indus basin is the most meltwater-dependent.
- Two-phase impact: near-term flood surplus and GLOF risk, long-term post-'peak water' decline in dry-season flows.
- GLOF case law: Kedarnath 2013, Chamoli 2021, South Lhonak (Sikkim) 2023 destroying Teesta-III dam.
- Irrigation and groundwater: reduced lean flows squeeze rabi cropping and intensify groundwater mining in the Indo-Gangetic plain.
- Hydropower vulnerability from erratic discharge and sediment loads; drying Himalayan springs (NITI Aayog: nearly 50%).
- Adaptation: cryosphere monitoring, early-warning systems, NMSHE, transboundary basin cooperation, demand management.
Concrete cases, schemes and judgments
- ICIMOD Hindu Kush Himalaya Assessment (2019) and HKH water report (2023)
- Chamoli disaster (February 2021) destroying Tapovan-Vishnugad project
- South Lhonak glacial lake outburst, Sikkim (October 2023)
- Shimla water crisis (2018)
- NITI Aayog report on drying Himalayan springs (2018)
Terminology to weave into the answer
Third Polepeak waterGLOFmeltwater dependenceNMSHEcryosphere