REMOTE SENSING AND GLACIER LAKES - ENVIRONMENT

News: ISRO tracks notable expansion of glacial lakes in Indian Himalayas

 

What's in the news?

       Recently, the Indian Space Research Organisation (ISRO) unveiled a satellite-data-driven analysis regarding the enlargement of glacial lakes within the catchment areas of the Indian Himalayan River basins.

 

Key takeaways:

       ISRO conducted an analysis of satellite data archives spanning four decades to examine changes in the glaciated environment.

       Long-term satellite imagery covering the catchments of Indian Himalayan River basins, extending from 1984 to 2023, was utilized in the study.

 

Key Highlights of ISRO's Study on Glacial Lakes:

       ISRO's data revealed a notable increase in the size of glacial lakes.

       Out of 2,431 lakes larger than 10 hectares identified during 2016-17, 676 glacial lakes exhibited significant expansion since 1984.

       Of these expanded lakes, 130 are located in India, distributed across the Indus, Ganga, and Brahmaputra river basins.

       The expansion of these lakes is attributed to the accelerating retreat of glaciers caused by global warming.

 

Glacial Lakes:

       Glacial lakes are bodies of water formed in depressions or basins created by the erosive action of glaciers.

       They are commonly found in regions where glaciers once existed or are currently present.

       These lakes vary in size and shape, ranging from small ponds to large, deep bodies of water.

 

Classification:

ISRO categorized glacial lakes into four main types based on their formation processes such as

       Moraine-dammed

       Ice-dammed

       Erosion-based

       Others

 

Formation Mechanisms:

1. Glacial Erosion:

       Glaciers erode and shape the landscape, creating depressions and basins.

 

2. Deposition of Glacial Moraines:

       Sediment and debris carried by glaciers form natural dams, blocking water flow and creating depressions for lake formation.

 

3. Melting Ice:

       Rising temperatures or glacier retreat leads to the melting of ice, filling depressions with water and forming glacial lakes.

 

4. Terminal Moraine Formation:

       Glaciers deposit sediment at their terminus, creating dams that impound water and form terminal moraine lakes.

 

Use of Remote-Sensing Technology:

       Monitoring glacial lakes in the Himalayan region is challenging due to rugged terrain, making satellite remote sensing a valuable tool.

       Satellite data analysis allows for tracking changes in glacial lakes over time, aiding in understanding their environmental impact and developing strategies to manage risks like glacial lake outburst floods and adapt to climate change.

 

Risk Mitigation Strategies:

       Lowering lake levels by 10 to 30 meters can significantly reduce the impacts of downstream flooding.

       Syphoning off lake water using long High-Density Polyethylene (HDPE) pipes is one effective method employed for risk mitigation.

       In 2016, the Sikkim State Disaster Management Authority utilized this approach to lower water levels in South Lhonak Lake.