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<p>Overshooting global warming targets risks irreversible Earth system changes. However, uncertainties remain in how critical Earth system components such as permafrost and the Atlantic Meridional Overturning Circulation (AMOC) respond to and interact under warming. By using three climate models of varying complexity to assess the permafrost carbon response under idealized climate mitigation and overshoot scenarios, we here show that permafrost loses 11–21 PgC of carbon per 100 degree-years of warming exposure (cumulative warming over 100 years) during temperature overshoot in a robust linear relationship. This relationship also holds true under relative Northern Hemisphere cooling from a temporary AMOC slowdown during temperature overshoot. This relative cooling partially offsets climate change impacts on permafrost, while in itself causing adverse impacts on climate and society. These results underscore the importance of including both destabilizing and stabilizing Earth system feedbacks when assessing overshoot impacts, critical for informing carbon budgets, net-zero planning, and climate change reversibility.</p>

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Permafrost carbon release scales linearly with overshoot warming mediated by AMOC tipping

  • 期刊论文

  • 出版模式：

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  • 发表日期：

    2026年7月16日

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  • Norman Julius Steinert,
  • Jörg Schwinger,
  • Eleanor Burke,
  • Biqing Zhu,
  • Thomas Gasser,
  • Gregory Munday,
  • Camilla Mathison,
  • So-Won Park,
  • Hanna Lee

摘要

Overshooting global warming targets risks irreversible Earth system changes. However, uncertainties remain in how critical Earth system components such as permafrost and the Atlantic Meridional Overturning Circulation (AMOC) respond to and interact under warming. By using three climate models of varying complexity to assess the permafrost carbon response under idealized climate mitigation and overshoot scenarios, we here show that permafrost loses 11–21 PgC of carbon per 100 degree-years of warming exposure (cumulative warming over 100 years) during temperature overshoot in a robust linear relationship. This relationship also holds true under relative Northern Hemisphere cooling from a temporary AMOC slowdown during temperature overshoot. This relative cooling partially offsets climate change impacts on permafrost, while in itself causing adverse impacts on climate and society. These results underscore the importance of including both destabilizing and stabilizing Earth system feedbacks when assessing overshoot impacts, critical for informing carbon budgets, net-zero planning, and climate change reversibility.