• The world could be heading towards a cascade of climate tipping points.
  • In an interconnected climate system, passing one tipping point may trigger a cascade of irreversible changes.
  • As the world continues to warm, some call for urgent global action to avert an “existential threat to civilization.”

We may be about to pass – or may already have passed – tipping points in the Earth’s climate, according to a group of leading scientists.

The scientists analyzed evidence on these nine components of our climate system – called “tipping points” because they are under growing threat of abrupt and irreversible changes.

1. Amazon rainforest

2. Arctic sea ice

3. Atlantic circulation

4. Boreal forests

5. Coral reefs

6. Greenland ice sheet

7. Permafrost

8. West Antarctic ice sheet

9. Part of East Antarctica

Passing one of these climate tipping points – from the collapse of the West Antarctic ice sheet to the loss of coral reefs and the Amazon rainforest – may increase the risk of crossing others, the scientists write in a commentary article in the journal Nature.

Ocean and atmospheric circulation and feedback between these interconnected climate shifts could accelerate the warming process, they warn, triggering a cascade of tipping points or even to a global tipping point – and a less habitable, “hothouse” Earth.

The world's climate tipping points are connected.
These are the world’s climate tipping points – and we’re getting close to the point of no return.
Image: Nature

Climate tipping points: a dominoes

How might such a climatic collapse happen? The authors point to the loss of Arctic sea-ice and the melting of Greenland’s ice sheet driving fresh water into the North Atlantic. They say this could have contributed to a 15% slowdown since the mid-20th century of the Atlantic Meridional Overturning Circulation (AMOC), a system of ocean currents that moves warm water northwards.

“Rapid melting of the Greenland ice sheet and further slowdown of the AMOC could destabilize the West African monsoon, triggering drought in Africa’s Sahel region,” they write.

“A slowdown in the AMOC could also dry the Amazon, disrupt the East Asian monsoon and cause heat to build up in the Southern Ocean, which could accelerate Antarctic ice loss.”

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In their opinion, the West Antarctic ice sheet might already have passed a tipping point.

The “grounding line” at which ice, ocean and bedrock meet in a glacial system called the Amundsen Sea Embayment is retreating irreversibly.

Its collapse could destabilize the rest of the West Antarctic ice sheet like “toppling dominoes,” according to one computer model study, and lead to about 3 metres of sea-level rise “on a timescale of centuries to millennia.”

The latest research suggests the Wilkes Basin, which is part of the East Antarctic ice sheet, might be similarly unstable – which could add another 3-4 metres to sea level a century or more from now.

‘An existential threat to civilization’

Some scientists disagree with the global climate tipping points argument and say it is speculation.

But the authors, led by Timothy Lenton, Professor of Climate Change and Earth System Science at the UK’s University of Exeter, argue that, despite the uncertainty, the stakes are so high it’s too risky to bet against.

They say “to err on the side of danger is not a responsible option,” and call for an international emergency response.

climate-tipping-points-will-cause-irreversible-changes-in-climate-system
Climate tipping points will cause irreversible changes in climate system
Image: Nature

“If damaging tipping cascades can occur and global climate tipping points cannot be ruled out, then this is an existential threat to civilization. No amount of economic cost–benefit analysis is going to help us. We need to change our approach to the climate problem.”

Two decades ago, scientists thought it would take a rise in global average surface temperature of 5°C above pre-industrial levels to reach climate tipping points. Recent Intergovernmental Panel on Climate Change (IPCC) reports suggesting this could occur between 1°C and 2°C.

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