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David B. :SetouchiExplorer: boosted
PIK_climate
PIK_climate
@PIK_climate@wisskomm.social  ·  activity timestamp 2 weeks ago

Several Earth system components may be closer to destabilisation than previously thought. Crossing critical temperature thresholds could trigger powerful feedback loops - pushing the planet toward a “ #Hothouse Earth” trajectory.

A commentary, published in One Earth with contributions from Oregon State University, PIK and IIASA, reviews climate feedbacks and 16 tipping elements that risk losing stability as warming continues.

▶️ https://youtu.be/xxeTyuwAdBc
➡️ Commentary: https://www.sciencedirect.com/science/article/pii/S2590332225003914?via%3Dihub

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PIK_climate
PIK_climate
@PIK_climate@wisskomm.social  ·  activity timestamp 2 weeks ago

Several Earth system components may be closer to destabilisation than previously thought. Crossing critical temperature thresholds could trigger powerful feedback loops - pushing the planet toward a “ #Hothouse Earth” trajectory.

A commentary, published in One Earth with contributions from Oregon State University, PIK and IIASA, reviews climate feedbacks and 16 tipping elements that risk losing stability as warming continues.

▶️ https://youtu.be/xxeTyuwAdBc
➡️ Commentary: https://www.sciencedirect.com/science/article/pii/S2590332225003914?via%3Dihub

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O=C=O
O=C=O
@tuxom@climatejustice.social  ·  activity timestamp 2 weeks ago

The risk of a hothouse Earth trajectory

Earth’s #climate is now departing from the stable conditions that supported human civilization for millennia. Crossing critical temperature thresholds may trigger self-reinforcing #feedbacks and tipping dynamics that amplify warming and destabilize distant #Earth system components. Uncertain tipping thresholds make precaution essential, as crossing them could commit the planet to a #hothouse trajectory with long-lasting and potentially irreversible consequences.

https://www.cell.com/one-earth/fulltext/S2590-3322(25)00391-4?_returnURL=https%3A%2F%2Flinkinghub.elsevier.com%2Fretrieve%2Fpii%2FS2590332225003914%3Fshowall%3Dtrue

#ClimateScience
#ClimateCrisis
#TippingPoint
#HothouseEarth

(A) The Earth’s current state (globe shown in black) is nearing tipping point thresholds (within yellow band). The yellow dot depicts a tipping point threshold, and the blue and red vertical bands on the left and right of the graphs indicate troughs that represent relatively stable cooler or hothouse Earth states, respectively. Depending on the tipping threshold, a small increase in warming could still allow for a transition back to a cool, stabilized Earth (orange arrow in upper graph) or place the Earth system on a hothouse trajectory (orange arrow in lower graph). If a critical tipping point threshold is crossed at a relatively low temperature, then a hothouse trajectory could occur even assuming fairly low future emissions. The tipping point window reflects the uncertainty of the tipping point temperature threshold.
(B) Case study scenario of interconnected feedbacks and tipping cascades linking Arctic and Atlantic processes to the Amazon. Warming from greenhouse gas emissions accelerates Arctic sea ice and Greenland Ice Sheet loss, reducing albedo and adding meltwater that weakens the Atlantic Meridional Overturning Circulation. A weakened AMOC shifts tropical rainfall patterns, increasing drought risk and potential dieback in the northern Amazon forest, further amplifying global warming through the feedback involving carbon loss. Note that once one tipping point is crossed, it will likely impact the timing and temperature thresholds for other tipping points.
(A) The Earth’s current state (globe shown in black) is nearing tipping point thresholds (within yellow band). The yellow dot depicts a tipping point threshold, and the blue and red vertical bands on the left and right of the graphs indicate troughs that represent relatively stable cooler or hothouse Earth states, respectively. Depending on the tipping threshold, a small increase in warming could still allow for a transition back to a cool, stabilized Earth (orange arrow in upper graph) or place the Earth system on a hothouse trajectory (orange arrow in lower graph). If a critical tipping point threshold is crossed at a relatively low temperature, then a hothouse trajectory could occur even assuming fairly low future emissions. The tipping point window reflects the uncertainty of the tipping point temperature threshold. (B) Case study scenario of interconnected feedbacks and tipping cascades linking Arctic and Atlantic processes to the Amazon. Warming from greenhouse gas emissions accelerates Arctic sea ice and Greenland Ice Sheet loss, reducing albedo and adding meltwater that weakens the Atlantic Meridional Overturning Circulation. A weakened AMOC shifts tropical rainfall patterns, increasing drought risk and potential dieback in the northern Amazon forest, further amplifying global warming through the feedback involving carbon loss. Note that once one tipping point is crossed, it will likely impact the timing and temperature thresholds for other tipping points.
(A) The Earth’s current state (globe shown in black) is nearing tipping point thresholds (within yellow band). The yellow dot depicts a tipping point threshold, and the blue and red vertical bands on the left and right of the graphs indicate troughs that represent relatively stable cooler or hothouse Earth states, respectively. Depending on the tipping threshold, a small increase in warming could still allow for a transition back to a cool, stabilized Earth (orange arrow in upper graph) or place the Earth system on a hothouse trajectory (orange arrow in lower graph). If a critical tipping point threshold is crossed at a relatively low temperature, then a hothouse trajectory could occur even assuming fairly low future emissions. The tipping point window reflects the uncertainty of the tipping point temperature threshold. (B) Case study scenario of interconnected feedbacks and tipping cascades linking Arctic and Atlantic processes to the Amazon. Warming from greenhouse gas emissions accelerates Arctic sea ice and Greenland Ice Sheet loss, reducing albedo and adding meltwater that weakens the Atlantic Meridional Overturning Circulation. A weakened AMOC shifts tropical rainfall patterns, increasing drought risk and potential dieback in the northern Amazon forest, further amplifying global warming through the feedback involving carbon loss. Note that once one tipping point is crossed, it will likely impact the timing and temperature thresholds for other tipping points.
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