UPSC MainsGEOGRAPHY-PAPER-I202510 Marks150 Words
हिंदी में पढ़ें
Q1.

Answer the following in about 150 words each: (a) Explain the causes of glacial lake outburst flood.

How to Approach

To answer this question effectively, one should begin by defining Glacial Lake Outburst Floods (GLOFs) and providing context about their increasing frequency. The body of the answer should then systematically detail the various natural and anthropogenic causes of GLOFs, categorizing them for clarity (e.g., climate change-related, geological, external triggers). Specific examples of each cause should be included. The conclusion should briefly summarize the multi-faceted nature of GLOF causes.

Model Answer

0 min read

Introduction

A Glacial Lake Outburst Flood (GLOF) is a sudden and catastrophic release of a significant volume of water from a glacial lake, often resulting in devastating downstream flooding. These lakes are typically impounded by unstable natural dams of moraine or ice. The increasing frequency and intensity of GLOFs, particularly in regions like the Himalayas, are a critical environmental concern, largely attributed to the accelerated glacial melt driven by climate change. A 2023 study highlighted that 15 million people are at risk globally from GLOFs, with a significant portion in Asian countries like India, China, Nepal, and Pakistan.

Causes of Glacial Lake Outburst Floods (GLOFs)

GLOFs are complex natural hazards triggered by a combination of factors that compromise the integrity of the natural dams holding glacial lakes. These causes can be broadly categorized as follows:

1. Climate Change and Glacial Retreat:

  • Increased Meltwater: Rising global temperatures lead to rapid melting of glaciers, which in turn increases the volume of water flowing into glacial lakes, causing them to expand rapidly in size and depth. This heightened water pressure can stress the dam.
  • Formation of New Lakes: As glaciers retreat, they often leave behind depressions that fill with meltwater, forming new, often unstable, glacial lakes.
  • Permafrost Thaw: Thawing permafrost can destabilize slopes and moraine dams, making them more susceptible to collapse.

2. Moraine or Ice Dam Instability:

  • Structural Weakness: Moraine dams, composed of unconsolidated sediment and debris, are inherently unstable. Over time, erosion, seepage, and the sheer pressure of increasing lake water can weaken their structure. Ice dams can also fail due to thermal stress, internal melting, or water pressure.
  • Glacier Surging: A sudden acceleration of a glacier's flow (glacial surging) can create new lakes or expand existing ones, leading to increased pressure on the dam.
  • Overtopping: When the lake water level rises too high, it can overtop the dam, leading to rapid erosion and eventual breach.

3. External Triggers:

  • Avalanches and Landslides: Large volumes of rock, ice, or snow avalanching or sliding into a glacial lake can create a displacement wave (seiche wave) that overtop and erode the dam.
  • Seismic Activity: Earthquakes or cryoseisms (icequakes) in tectonically active mountainous regions can cause sudden structural changes, weakening or rupturing moraine and ice dams.
  • Heavy Rainfall or Rapid Snowmelt: Extreme precipitation or exceptionally fast snowmelt can rapidly increase the lake's volume, intensifying pressure on the dam and potentially leading to overtopping or internal erosion.
  • Volcanic Eruptions: While less common in the Himalayas, volcanic or geothermal activity beneath a glacier can cause rapid melting and lake formation, leading to dam failure.

4. Anthropogenic Factors:

  • Infrastructure Development: Unregulated construction of roads, dams, and hydropower projects near glacial lakes can disturb fragile slopes and alter drainage patterns, increasing GLOF risk. For instance, the 2023 Sikkim GLOF severely impacted the Teesta III Dam.
  • Greenhouse Gas Emissions: Human-induced greenhouse gas emissions are the primary driver of climate change, directly contributing to accelerated glacial melt and the expansion of glacial lakes.

Conclusion

In conclusion, Glacial Lake Outburst Floods are primarily driven by the dynamic interplay of climate change-induced glacial melt, inherent geological instability of glacial dams, and external environmental triggers. The escalating threat of GLOFs, particularly in vulnerable regions like the Himalayas, underscores the urgent need for comprehensive monitoring, early warning systems, and robust disaster management strategies. Addressing global climate change and implementing sustainable development practices are crucial steps to mitigate the risks associated with these devastating natural phenomena.

Answer Length

This is a comprehensive model answer for learning purposes and may exceed the word limit. In the exam, always adhere to the prescribed word count.

Additional Resources

Key Definitions

Glacial Lake Outburst Flood (GLOF)
A GLOF is a sudden release of a significant amount of water retained in a glacial lake, which has formed either at the side, in front, within, beneath, or on the surface of a glacier, often due to the failure of its natural moraine or ice dam.
Moraine Dam
A moraine dam is a natural embankment formed by unconsolidated glacial till (debris, rock, and sediment) deposited by a retreating glacier, which can impound meltwater to create a glacial lake.

Key Statistics

A 2023 study found that 15 million people globally are at risk from GLOFs, with a majority in China, India, Nepal, Pakistan, and Peru. In the Hindu Kush Himalaya region, nearly 1 million people live within 10 km of a glacial lake.

Source: UN University, The New Indian Express (2024-09-18), Wikipedia (2023 study)

The area of glacial lakes in the Hindu Kush Himalaya (HKH) region has increased at a rate of approximately 22% per decade between 1990 and 2020 due to climate change-driven glacial melt.

Source: The New Indian Express (2024-09-18)

Examples

South Lhonak Lake GLOF (Sikkim, India)

In October 2023, the South Lhonak Lake in Sikkim experienced a catastrophic GLOF. The event, driven by glacial melt and permafrost thaw, resulted in a tsunami-like wave that breached the lake, causing massive downstream flooding, killing 55 people, and destroying the 1200 MW Teesta III hydropower dam at Chungthang.

Chorabari GLOF (Kedarnath, India)

The 2013 Chorabari GLOF, exacerbated by cloudbursts and landslides, triggered the devastating Kedarnath floods. This event caused significant casualties and widespread infrastructure damage, highlighting the compounding effects of multiple natural hazards.

Frequently Asked Questions

How does climate change specifically contribute to GLOFs?

Climate change accelerates glacier melting, increasing the volume of water in existing glacial lakes and leading to the formation of new ones. This added water pressure and the instability caused by thawing permafrost weaken the natural dams, making them more prone to failure.

Are all glacial lakes dangerous?

No, not all glacial lakes are dangerous. The risk depends on factors like the stability of the dam (moraine or ice), the volume of water, the lake's location, and the topography of the downstream area. However, many lakes in geologically active and rapidly warming regions are identified as high-risk.

Topics Covered

Physical GeographyEnvironmental ScienceGlaciologyHydrologyNatural Disasters