·The Hindu·15 marks·250–350 words

Discuss why hydropower development in the Hindu Kush Himalaya region is increasingly vulnerable to climate-induced cryosphere hazards. Suggest risk-informed planning measures.

In this answer
  1. Why vulnerability is rising
  2. Risk-informed planning measures

ICIMOD's 2026 assessment records that Hindu Kush Himalaya (HKH) glaciers lost about 12% of their area between 1990 and 2020, with ice loss rates doubling since 2000 [1]. Hydropower in the region is therefore being built against a non-stationary hazard baseline, as the August 2026 Bhote Koshi–Trishuli flood showed.

Why vulnerability is rising

  • Destabilising cryosphere: glacier retreat and permafrost thaw weaken bedrock and moraines, raising the frequency of ice-rock avalanches and GLOFs [1].
  • Cascading hazard chains: at Rasuwa an ice-rock avalanche dammed the Lhende river, and the breach surge carried water, sediment and boulders far downstream [2] — leaving an estimated 2.2 million tonnes of debris [3]. Damage came from debris, not water alone.
  • Siting and concentration of assets: run-of-river plants cluster in steep, glacier-fed headwater corridors, so a single detachment disables operating and under-construction capacity in one basin — as at Chamoli (2021) and South Lhonak, Sikkim (2023).
  • Underpriced risk: design return periods fixed at financial close age rapidly; World Bank Lifelines values annual hazard damage to power and transport in developing countries at $18 billion, but user disruption at $390 billion — a cost no project IRR captures [5].
  • Protection finance lags hazard: Nepal's ~$50 million GCF glacier-risk project was approved only in July 2025, years after conception [6].

Risk-informed planning measures

  • Shift from project-level clearance to cumulative, basin-scale hazard assessment of cryosphere risk.
  • Scale satellite monitoring, lake-lowering and automated early warning, as under India's GLOF Risk Mitigation Programme covering high-risk lakes among ~7,500 Himalayan lakes [4].
  • Design for sediment and debris loads — larger spillways, freeboard, desilting — and avoid the highest-hazard headwater reaches.
  • Institutionalise transboundary data-sharing with ICIMOD and riparian neighbours for basin-wide warning [2].
  • Build risk transfer and contingency finance into project appraisal, and fast-track adaptation funding.

Himalayan hydropower remains essential to South Asia's clean-energy transition; the task is to build it on honest hazard arithmetic. Aligning siting, design and finance with a warming cryosphere would make hydropower genuinely resilient and advance SDG-7 and SDG-13 together.

Sources

  1. 1ICIMOD — HKH glaciers losing ice at double the rate since 2000 (2026)12% glacier area loss 1990–2020; ice-loss rate doubled post-2000
  2. 2ICIMOD — Kyirong-Rasuwa Flood 2026, Nepal-China cryosphere riskice-rock avalanche damming the Lhende, downstream surge, transboundary monitoring
  3. 3UNDP — Nepal floods: 2.2 million tonnes of debris estimated (2026)scale of debris deposition
  4. 4PIB, Ministry of Home Affairs — Glacial Lake Outburst Flood MitigationNDMA GLOF Risk Mitigation Programme, high-risk lakes, ~7,500 Himalayan glacial lakes
  5. 5World Bank/GFDRR — *Lifelines: The Resilient Infrastructure Opportunity* (2019)$18 bn asset damage vs $390 bn user-disruption cost
  6. 6Green Climate Fund — FP272: Protecting livelihoods and assets from GLOFs in Nepalapproval date and size of Nepal's glacier-risk project

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