How might Climate Tipping Points affect us?

There are many potential tipping points in the climate system that scientists are worried about, many of which could affect a lot of people. Here’s some of them:

Lenton 2008 Map.png
Map (and examples) from Lenton et al (2008), Tipping elements in the Earth’s climate system , PNAS, 2008, 105 (6) 17861793. Copyright (2008) National Academy of Sciences.
  • Ice sheet collapse
    • Many ice sheets (especially in West Antarctica) are grounded at sea on prominent underwater ridges. Once warming seas melt the ice past these ridges these ice sheets can be melted from underneath as well as from the top and sides, which could cause a tipping point in ice sheet melting. This could cause a similarily rapid jump in sea levels
  • Arctic sea ice loss
    • As described in ‘What are Climate Tipping Points?‘, less sea ice due to warming results in a darker sea surface overall, which reflects less heat, raises local temperatures, and leads to yet more sea ice loss and warming. This would cause warming to happen far faster in the Arctic than anywhere else, and it’s been suggested that this could cause stranger weather elsewhere by affecting the jet stream
  • Gulf Stream slowdown
    • Ocean circulation in the North Atlantic (known as the Atlantic Meridional Overturning Circulation, of which the Gulf Stream forms a part) is gradually slowing down as meltwater from Greenland enters the Ocean, and it could pass a tipping point beyond which it slows down even more rapidly. This would mean less warmth for northern Europe as well as higher sea levels in eastern US as water ‘builds up’ there instead of moving north
  • Amazon dieback
    • Decreasing rainfall could push the Amazon rainforest past a tipping point beyond which the rainforest ecosystem can no longer be maintained and a rapid switch to savanna could occur. This would also lead to a large release of carbon that used to be locked up in the rainforest and so could worsen global climate change
  • Monsoon weakening
    • Changing albedo (how much light and heat is reflected by the Earth’s surface) in South Asia could cause a rapid weakening of the Indian Summer Monsoon that could could cause severe droughts across South Asia
  • Permafrost / clathrate thawing
    • A lot of methane is trapped frozen in seafloor sediments and in permafrosts on land. Global warming could cause these deposits to melt, and beyond a melting tipping point large volumes of methane could rapidly escape and add to global carbon emissions (and then trigger more methane release). However, we currently do not know how much warming is needed to trigger this

It is critical to try and predict when we might reach these tipping points so that we can try and avoid them – visit  ‘Can we predict Climate Tipping Points?‘ to find out how scientists are trying to do this.