Geography

Glacial Lake Outburst Floods (GLOFs)

Why in news — In early July 2025, Nepal experienced several glacial lake outburst floods that destroyed a Chinese‑built bridge and damaged hydropower projects. These incidents heightened concern about similar risks in the Indian Himalayas as rising temperatures melt glaciers and enlarge glacial lakes.

Why in news?

In early July 2025, Nepal experienced several glacial lake outburst floods that destroyed a Chinese‑built bridge and damaged hydropower projects. These incidents heightened concern about similar risks in the Indian Himalayas as rising temperatures melt glaciers and enlarge glacial lakes.

What are GLOFs?

  • A glacial lake outburst flood occurs when a natural dam of ice or loose moraine holding back a lake collapses suddenly, releasing large volumes of water. These floods are high‑velocity and can devastate downstream communities, infrastructure and ecosystems.

Causes

  • Climate change: Warming temperatures accelerate glacial retreat and lead to the formation of unstable lakes. Over 7,500 glacial lakes exist in India, many above 4,500 metres.
  • Avalanches and landslides: Ice or rock falling into a lake can displace water and trigger a breach. Avalanches were implicated in the 2023 South Lhonak lake disaster in Sikkim.
  • Heavy rainfall and cloudbursts: Intense monsoon downpours rapidly raise lake levels, stressing weak dams. The 2013 Kedarnath tragedy in Uttarakhand was linked to a cloudburst and subsequent GLOF.
  • Seismic activity: Earthquakes can destabilise dams and trigger collapse, especially in seismically active zones like Uttarakhand and northeastern India.
  • Human activities: Unregulated construction of roads and hydropower projects near glacier zones and climate‑warming emissions add to the risk.

Types of glacial lakes

  • Supraglacial lakes: Pools that form on the surface of a glacier. They are prone to sudden drainage during summer melt.
  • Moraine‑dammed lakes: Lakes held back by unconsolidated debris at the terminus of a glacier. Such lakes are unstable because the dams are weak and easily eroded.

Impacts

  • Loss of life and property: GLOFs can inundate villages, damage roads, bridges and hydropower stations and displace communities.
  • Environmental effects: Sudden influxes of water and debris raise riverbeds, alter courses and destroy habitats.

Response and mitigation

  • National strategies: India’s National Disaster Management Authority has identified 195 high‑risk glacial lakes and initiated programmes to install automated weather stations, early warning systems and artificial drainage channels.
  • Technological measures: Techniques like Synthetic Aperture Radar interferometry monitor glacier slopes, while electrical resistivity tomography helps map ice cores beneath moraine dams.
  • Community involvement: Local communities are trained to monitor lakes, report anomalies and respect religious sensibilities when implementing structural measures.

Significance

  • GLOFs highlight the cascading risks of climate change in the Himalayas. Studying and mitigating them is essential for protecting lives and infrastructure.
  • Efforts to manage GLOFs also contribute to building resilience in mountain states and complement India’s broader climate‑adaptation strategies.

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