Climate Change Impact on India and World – International Reports, Key Observations, etc.

Thwaites Glacier

Note4Students

From UPSC perspective, the following things are important :

Prelims level : Thwaites Glacier

Mains level : Sea level rise and its impact

 

In the Antarctic floats a massive glacier, roughly the size of Britain, whose melting has been a cause of alarm for scientists over the years. Now, a new study has pinned the cause of the melting to the presence of warm water at a vital point beneath the glacier.

Thwaites Glacier

  • The Thwaites Glacier is 120 km wide at its broadest, fast-moving and melting fast over the years.
  • Because of its size (1.9 lakh square km), it contains enough water to raise the world sea level by more than half a metre.
  • Studies have found the amount of ice flowing out of it has nearly doubled over the past 30 years. Today, Thwaites’s melting already contributes 4% to global sea level rise each year.
  • It is estimated that it would collapse into the sea in 200-900 years. Thwaites is important for Antarctica as it slows the ice behind it from freely flowing into the ocean.
  • Because of the risk it faces — and poses — Thwaites is often called the Doomsday Glacier.

What has the new study found?

  • A 2019 study had discovered a fast-growing cavity in the glacier.
  • More recently researchers detected warm water at a vital point below the glacier.
  • Scientists dug a 600-m-deep and 35-cm-wide access hole, and deployed an ocean-sensing device called Icefin to measure the waters moving below the glacier’s surface.
  • The study reported water at just two degrees above freezing point at Thwaites’s “grounding zone” or “grounding line”.

What is the grounding line?

  • The grounding line is the place below a glacier at which the ice transitions between resting fully on bedrock and floating on the ocean as an ice shelf.
  • The location of the line is a pointer to the rate of retreat of a glacier.
  • When glaciers melt and lose weight, they float off the land where they used to be situated. When this happens, the grounding line retreats.
  • That exposes more of a glacier’s underside to seawater, increasing the likelihood it will melt faster.
  • This resulted in the glacier speeding up, stretching out, and thinning, causing the grounding line to retreat ever further.
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