GS Paper 1 10 marks · 150w 9 min Medium
Bring out the relationship between the shrinking Himalayan glaciers and the symptoms of climate change in the Indian sub-continent.
Subtopic: Geography · Himalayan glaciers and climate change
How to structure your answer
Introduction: HKH warming faster than global average; glaciers as the visible link → Shrinkage as a symptom: elevation-dependent warming, declining snowfall, black carbon; ICIMOD one-third-loss warning → Shrinkage as a driver: GLOFs (Kedarnath, Chamoli, South Lhonak), altered Indus–Ganga–Brahmaputra regimes, water and hydropower insecurity → Ecosystem shifts: snowline, treeline, springs → Conclusion: glacier retreat as the subcontinent's climate thermometer
Detailed model answer
197 words · target 150 words · 9 min
The Hindu Kush Himalaya is warming faster than the global average, and its shrinking glaciers are both a symptom of climate change in the subcontinent and a driver of its further symptoms.
Glacier shrinkage as a symptom
- Elevation-dependent warming, declining snowfall and more rain falling instead of snow have cut glacier accumulation; Gangotri and most central and eastern Himalayan glaciers are in sustained retreat.
- Black carbon and dust from the Indo-Gangetic plain darken ice surfaces and accelerate melt — a direct human fingerprint.
- The ICIMOD Hindu Kush Himalaya Assessment warns that roughly one-third of glacier volume could be lost by 2100 even if warming is held to 1.5°C.
Shrinkage as a driver of further symptoms
- Expanding proglacial lakes raise glacial lake outburst flood risk — Kedarnath (2013), Chamoli (2021) and the South Lhonak GLOF in Sikkim (2023) that destroyed the Teesta-III dam.
- The regimes of the Indus, Ganga and Brahmaputra are shifting — higher meltwater flows in the near term, then long-term decline, threatening irrigation, hydropower and the water security of hundreds of millions.
- Rising snowlines and treelines and drying mountain springs disturb Himalayan ecosystems and livelihoods.
Glacier retreat is thus the subcontinent’s most visible climate thermometer and its earliest warning of a water-insecure future.
What an examiner expects to see
- Frame the relationship as two-way: glacier shrinkage is both an indicator of warming and a cause of downstream climate impacts
- Drivers of retreat: elevation-dependent warming, reduced snowfall, rain-on-snow events, black carbon deposition from the Indo-Gangetic plain
- Authoritative evidence: ICIMOD HKH Assessment — about one-third of glacier volume lost by 2100 even at 1.5°C warming
- GLOF hazard chain: proglacial lake expansion → Kedarnath 2013, Chamoli 2021, South Lhonak (Sikkim) 2023 destroying Teesta-III
- Hydrological consequence: 'peak water' then long-term decline in Indus–Ganga–Brahmaputra flows, hitting irrigation and hydropower
- Ecosystem symptoms: rising snowline and treeline, drying springs, livelihood stress for mountain communities
Concrete cases, schemes and judgments
- Gangotri glacier's documented sustained retreat over recent decades
- South Lhonak lake GLOF, October 2023, which wrecked the 1,200 MW Teesta-III hydropower dam in Sikkim
- Chamoli disaster, February 2021 — rock-ice avalanche destroying the Rishiganga and Tapovan projects
- ICIMOD Hindu Kush Himalaya Assessment (2019) one-third glacier-loss projection
- Kedarnath flash floods of June 2013 linked to Chorabari lake breach
Terminology to weave into the answer
Hindu Kush Himalayaglacial lake outburst floodelevation-dependent warmingblack carbonpeak watercryosphere