Assessing the risk of climate 'overshoots'

Publicly released:
International
PHOTO: Pixabay
PHOTO: Pixabay

New research has looked into the feasibility of reversing global warming once temperatures have temporarily “overshot” the Paris 1.5 °C limit. The idea relies on future carbon removal technologies being available at scale in the future. However, the team found that after an overshoot, many aspects of the Earth system — such as biodiversity on land — may not bounce back to pre-overshoot levels. Sea levels would also continue to rise, even if temperatures decline following an overshoot. They conclude that rapidly reining in emissions is the best path forward to limiting climate changes.

Media release

From: Springer Nature

Concerns about the growing use and acceptance of overshoot scenarios, in which warming is allowed to temporarily increase past the Paris 1.5 °C limit, are raised in a paper published in Nature. The study indicates that reversing global warming following a climate overshoot may be difficult within the time frames envisioned in the present day. Instead, limiting rises in global temperatures are likely to be the most effective strategy to mitigate climate changes.

The Paris Agreement has established 1.5 °C warming beyond pre-industrial temperatures as  the long-term limit for global temperature increases. It has been proposed that temporarily exceeding this target, termed an overshoot, and then reversing subsequent warming to below 1.5 °C may be possible by  achieving net negative carbon  emissions (although this  will rely on the development of carbon capture technologies). However, the impacts of overshoots on climate change are unclear.

Carl-Friedrich Schleussner, Joeri Rogelj and colleagues explored modelling simulations of overshoot pathways and long-term climate stabilization. They find that the risk for global and regional climate changes differs between scenarios where overshoots do or do not happen. The authors suggest that temperature decline after an overshoot may  be more difficult than expected, owing to possible amplification of warming from strong Earth-system feedbacks, which may result in long-term warming.

Schleussner and colleagues found that following an overshoot, many aspects of the Earth system — such as species abundance, carbon stocks and biodiversity on land — may not return to pre-overshoot levels. They also highlight that sea levels will continue to rise, even if temperatures decline following an overshoot. The authors suggest that efforts to reduce global temperatures will be more likely to limit climate risks than attempting to stabilize global temperature rises resulting from overshoots.

Overshoot scenarios rely on the possibility that carbon dioxide removal technologies will be available at scale in the future. The authors indicate that any preventive carbon capture system that could be developed would need to remove in the region of several hundred gigatonnes of carbon  to protect against high-risk outcomes. However, current technical, economic and sustainability considerations may prevent a system operating at these levels.

The findings suggest that overconfidence in the controllability of changes following any overshoot should be avoided. They conclude that only rapid declines in emissions are effective in limiting climate changes.

Attachments

Note: Not all attachments are visible to the general public. Research URLs will go live after the embargo ends.

Research Springer Nature, Web page
Journal/
conference:
Nature
Research:Paper
Organisation/s: The University of Melbourne, International Institute for Applied Systems Analysis (IIASA), Austria
Funder: We acknowledge support from the Horizon 2020 research and innovation programmes of the European Union under grant agreement no. 101003687 (PROVIDE). G.G. acknowledges support from the Bundesministerium für Bildung und Forschung (BMBF) under grant agreement no. 01LS2108D (CDR PoEt). T.G. also acknowledges support from the Horizon 2020 and Horizon Europe research and innovation programmes of the European Union under grant agreement nos. 773421 (Nunataryuk) and 101056939 (RESCUE). J.S. is funded by the German Research Foundation (DFG) under Excellence Strategy of Germany—EXC 2037:CLICCS—Climate, Climatic Change, and Society—project no. 390683824, contribution to the Center for Earth System Research and Sustainability (CEN) of Universität Hamburg. The GFDL ESM2M simulations were conducted at the Swiss National Supercomputing Centre. B.S. acknowledges support from the Research Council of Norway under grant agreement no. 334811 (TRIFECTA).
Media Contact/s
Contact details are only visible to registered journalists.