Context: The National Disaster Management Authority (NDMA) has finalised a list of 189 “high-risk” glacial lakes for mitigation measures to reduce the risk emanating from them.
Glacial Lakes
- Formation: Created by meltwater accumulating in depressions left by retreating glaciers.
- Types: ISRO categorised glacial lakes into four types: moraine-dammed, ice-dammed, erosion-based, and others.
- Moraine-dammed lakes are formed by water dammed by debris left by glaciers.
- Ice-dammed lakes are formed by water dammed by ice.
- Erosion-based lakes are formed by water trapped in depressions created by erosion.
- Importance: Source of freshwater for rivers.
- Risks of Glacial Lakes:
- Glacial lake outburst floods (GLOFs) can have devastating consequences downstream.
- GLOFs occur when large volumes of meltwater are released due to dam failures.
- Dam failures can be triggered by avalanches or other factors.
Situation in Uttarakhand |
Uttarakhand has 13 glacial lakes that are susceptible to Glacial Lake Outburst Floods (GLOFs).
- 5 of these lakes, considered highly sensitive, fall into the ‘A’ category.
- These include Vasudhara Tal in the Dhauliganga basin and four lakes in Pithoragarh district: Maban Lake in Lassar Yangti Valley, Pyungru Lake in the Darma basin, and two unclassified lakes—one in the Darma basin and another in Kuthi Yangti Valley.
|
Glacial lake outburst floods (GLOFs)
- Definition: A GLOF is a flood that occurs when water dammed by a Glacial Moraine is released suddenly.
- Features of GLOF: Glacier Lake Outburst flood has three main features
- Involves sudden (and sometimes cyclic) releases of water.
- These are rapid events, lasting hours to days.
- These result in large downstream river discharges, which often result in catastrophic flooding or disasters
- Examples of GLOF-related disasters:
- 1926 Jammu and Kashmir deluge
- 1981 Kinnaur valley floods in Himachal Pradesh
- 2013 Kedarnath outburst in Uttarakhand
- 2023 Sikkim GLOF event: A combination of excess rainfall + series of earthquakes in Nepal may have caused the Sikkim GLOF event.
Reasons for Glacial Lake Outburst Floods (GLOFs)
- Melting of Glaciers: As global temperatures rise, glaciers are melting more quickly, causing glacial lakes to fill with water.
- The increased water level puts pressure on the lake’s natural boundaries, which are often made of unstable ice and debris.
- When these boundaries break, it can lead to a GLOF.
- Avalanches and Earthquakes: Landslides or ice avalanches near glacial lakes can push large amounts of water, causing the natural dams to burst and trigger a GLOF.
- Earthquakes can also destabilise the area, leading to a similar effect.
- Extreme Weather Conditions: Heavy rainfall, severe storms, or sudden changes in temperature can weaken the stability of glacial lakes, increasing the likelihood of a GLOF.
- Climate Change: The Himalayan-Hindukush region, which is highly affected by climate change, is seeing accelerated glacier melting.
- This leads to the formation of more glacial lakes, raising the risk of GLOFs.
- Climate change is also causing more frequent and intense cloudbursts, further contributing to GLOFs.
- Volcanic Activity: In regions near volcanoes, volcanic activity can heat glaciers and cause them to melt faster, increasing the risk of a GLOF.
- Weak Moraine Embankments: Moraines, which are piles of debris left by glaciers, often act as natural dams for glacial lakes.
- However, these moraines can be weak and prone to breaking, leading to GLOFs.
- Human Activities: Infrastructure projects like dams and roads in mountainous areas can add stress to the landscape, making GLOFs more likely.
- Example: 2021 Chamoli GLOF, which was linked to multiple hydroelectric projects in the area.
Reason For Vulnerabilities of GLOF in Himalayan Region |
The Himalayan states of India, such as Uttarakhand, Sikkim, and Himachal Pradesh, are highly vulnerable to GLOFs due to several factors:
- Expanding Glacial Lakes: ISRO’s satellite data from 1984 to 2023 shows that glacial lakes in the Indus, Ganga, and Brahmaputra basins have expanded significantly.
- Out of 2,431 lakes larger than 10 hectares, 676 have grown substantially, with 601 lakes more than doubling in size.
- Melting Glaciers: The Hindu Kush Himalayan Assessment report indicates that one-third of the region’s glaciers could melt, significantly increasing the risk of GLOFs.
- Geological Activity: The Indian tectonic plate is moving northward at a rate of about 2 cm per year, causing the Himalayas to rise by approximately 5 mm annually.
- This movement makes the region geologically active and structurally unstable, with frequent landslides and earthquakes that can trigger GLOFs.
- Human Impact: Large-scale human settlements and activities in the region have led to significant deforestation.
- This loss of forest cover reduces natural barriers that could help control floods, thereby exacerbating the impact of GLOFs.
|
Impacts of Glacial Lake Outburst Floods (GLOFs)
- Loss of Life and Property: GLOFs can lead to significant loss of life and destruction of property, including houses, bridges, roads, forests, and farmland, as well as livestock and crops.
- Example: GLOF in Sikkim, India, in October 2023 resulted in the deaths of at least 18 people and left over 150 missing.
- Similarly, a GLOF in Uttarakhand, India, in June 2013 claimed over 5,000 lives and caused extensive damage to hydropower projects.
- Disruption of Livelihoods: GLOFs can disrupt the livelihoods of local communities for extended periods by limiting their access to resources, markets, services, and opportunities.
- Additionally, GLOFs can harm the tourism industry, which is a critical source of income in many mountainous regions.
- Damage to Infrastructure and Environment: GLOFs can damage or destroy key infrastructure, such as hydropower plants, which are vital for electricity generation and reducing greenhouse gas emissions.
- GLOFs can also significantly alter the landscape, erode soil, increase sediment in rivers, and negatively impact water quality and availability.
Mitigating the Risks of Glacial Lake Outburst Floods (GLOFs)
- Identifying Potentially Dangerous Lakes: Identifying lakes that pose a high risk requires a multidisciplinary approach.
- This includes field observations, studying historical records, and analysing the geomorphological and geotechnical features of the area.
- Such information is crucial for prioritising monitoring efforts and implementing risk-reduction strategies.
- Use of Technology: Leveraging technology like synthetic-perture radar (SAR) imagery can significantly improve early warning systems.
- Satellite remote sensing is a valuable tool due to:
- Wide coverage
- Revisit capability
- Satellite data helps understand glacial lake dynamics for:
- Environmental impact assessment
- Developing strategies for:
- GLOF risk management
- Climate change adaptation
Fact
|
- There are nearly 7,500 glacial lakes in the Himalayan mountain ranges located in India and some of them are being monitored through remote sensing.
- However, fully assessing their impact is only possible with site visits, which is difficult owing to inhospitable terrain.
|
- Channelling Potential Floods: Structural management of lakes is key to reducing GLOF risks.
- Techniques such as controlled breaching, pumping out excess water, and constructing tunnels can help lower the water levels in lakes, thereby minimising the threat of a GLOF.
- These interventions must be carefully planned and executed to avoid adverse effects downstream.
- Uniform Codes for Construction Activity: Establishing uniform construction codes for infrastructure and land use in GLOF-prone areas is vital.
- These codes should account for geological and hydrological risks and incorporate mitigation measures into construction projects to ensure safety.
GLOF Risk Mitigation |
- A 2023 study modelled the impact of lowering water levels in Himachal Pradesh’s Ghepan Gath Lake to reduce risks for downstream Sissu town.
- Lowering lake levels by 10-30 metres significantly reduced, but didn’t eliminate, GLOF risks.
- One method to lower lake levels involves using High Density Polyethylene (HDPE) pipes.
- This method was used in 2016 to reduce water levels in Sikkim’s South Lhonak Lake.
|
- Enhancing Early Warning Systems (EWS): Early warning systems are essential for disaster preparedness.
- Implementing sensor-based and monitoring-based technical systems for GLOF early warnings can provide timely alerts to vulnerable communities.
- Expanding the reach of these systems is particularly important in areas prone to GLOFs.
- Training Local Manpower: Local communities are crucial in disaster response and preparedness.
- Training local personnel in GLOF response can enhance their ability to act swiftly and effectively.
- These trained individuals can lead search and rescue operations, help set up emergency shelters, and manage relief distribution, forming the first line of defence during disasters.
- Comprehensive Alarm Systems: Modern communication technologies, such as cell phones and smartphones, can complement or replace traditional alarm systems.
- Using these technologies for mass notification can ensure that timely warnings reach a broader audience, improving disaster response and preparedness.
Sharing is caring!