INDIA’S PREPAREDNESS AGAINST GLOF EVENTS
INDIA’S PREPAREDNESS AGAINST GLOF EVENTS
Introduction
Glacial Lake Outburst Floods (GLOFs) pose a serious and growing threat in the Indian Himalayan Region (IHR), particularly in light of accelerating glacial melt due to climate change. As witnessed in Nepal’s recent disasters, such events can cause devastating downstream damage to lives, infrastructure, and ecosystems. India, sharing similar high-altitude terrains, is increasingly focusing on mitigation and early warning mechanisms to prevent large-scale disasters. This essay explores India’s preparedness against GLOFs, the risks involved, and the institutional mechanisms in place to counter them.
Nature of GLOF Risk in India
-
Geographical Scope: The IHR contains over 28,000 glacial lakes and is spread across 11 river basins.
-
Types of Lakes:
-
Supraglacial Lakes: Formed on glaciers, especially vulnerable in warmer months.
-
Moraine-Dammed Lakes: Damed by unstable debris, prone to sudden rupture due to melting or external triggers like landslides.
-
-
Risk Triggers:
-
Ice and rock avalanches
-
Excessive meltwater pressure
-
Earthquakes and glacial seismic activity
-
-
Recent Catastrophes:
-
2023 Sikkim GLOF destroyed the Chungthang hydropower project.
-
2013 Kedarnath disaster, triggered by the Chorabari lake, caused widespread devastation.
-
Institutional Framework and NDMA’s Role
-
NDMA’s Strategic Shift:
-
Moving from reactive post-disaster response to risk mitigation through the Committee on Disaster Risk Reduction (CoDRR).
-
Coordination among scientific institutions, states, and UTs.
-
-
National GLOF Mitigation Programme:
-
Funded with $20 million, initially targeting 56 high-risk lakes, expanded to 195.
-
Risk categorisation into four levels based on hazard potential.
-
-
Objectives:
-
Hazard assessment and monitoring
-
Installation of Automated Weather and Water Stations (AWWS)
-
Early Warning Systems (EWS) in downstream areas
-
Engineering interventions (e.g., controlled draining, retention structures)
-
Community participation and awareness
-
Technological and Scientific Advances
-
Remote Sensing & SAR Interferometry:
-
Detects micro-changes in slopes using satellite imagery.
-
Key to understanding moraine dam stability.
-
-
Expedition Tools:
-
Bathymetry: To measure lake depth and volume.
-
Electrical Resistivity Tomography (ERT): Detects presence of ice-cores under moraine dams.
-
UAV Surveillance: For mapping and slope analysis.
-
-
Monitoring Stations:
-
Sikkim has piloted automated data collection every 10 minutes.
-
Data includes temperature, water level, and visual updates.
-
Gaps and Challenges
-
Access and Monitoring Limitations:
-
Most lakes are located above 4,500 m, limiting on-ground surveys.
-
Lack of all-weather monitoring stations due to remoteness and harsh conditions.
-
-
Data Deficiency:
-
Surface area analysis via satellite is post-facto, not predictive.
-
Few initiatives for real-time risk modelling.
-
-
Community Integration:
-
Local sentiments and religious significance of glacial lakes can impede surveys.
-
Need for trust-building and sensitisation during expeditions.
-
-
Trans-boundary Coordination:
-
Absence of early warning sharing between China and Nepal illustrates the urgency of regional protocols.
-
India faces similar vulnerabilities in border river systems.
-
Conclusion
India has made commendable strides in mapping, monitoring, and mitigating GLOF threats through institutional collaboration and technological innovation. However, challenges remain in terms of accessibility, predictive monitoring, and community integration. Future efforts must expand real-time systems, transboundary cooperation, and indigenous technology deployment to protect Himalayan communities from this escalating climate risk.
For classes, materials, test series and mentorship – contact us at +91 6366-294954
