地质记录
铅(地质)
气候系统
预警系统
气候突变
政权更迭
环境科学
气候变化
地球系统科学
全球变暖
环境资源管理
气候学
地质学
引爆点(物理)
地球科学
生态学
计算机科学
全球变暖的影响
生态系统
海洋学
古生物学
电信
工程类
电气工程
生物
作者
Victor Brovkin,Edward J. Brook,John W. Williams,Sebastian Bathiany,Timothy M. Lenton,C. Michael Barton,Robert M. DeConto,Jonathan F. Donges,Andrey Ganopolski,Jerry F McManus,Summer Praetorius,Anne de Vernal,Ayako Abe‐Ouchi,Hai Cheng,Martin Claußen,Michel Crucifix,Gilberto C. Gallopín,Virginia Iglesias,Darrell S. Kaufman,Thomas Kleinen
标识
DOI:10.1038/s41561-021-00790-5
摘要
The geological record shows that abrupt changes in the Earth system can occur on timescales short enough to challenge the capacity of human societies to adapt to environmental pressures. In many cases, abrupt changes arise from slow changes in one component of the Earth system that eventually pass a critical threshold, or tipping point, after which impacts cascade through coupled climate–ecological–social systems. The chance of detecting abrupt changes and tipping points increases with the length of observations. The geological record provides the only long-term information we have on the conditions and processes that can drive physical, ecological and social systems into new states or organizational structures that may be irreversible within human time frames. Here, we use well-documented abrupt changes of the past 30 kyr to illustrate how their impacts cascade through the Earth system. We review useful indicators of upcoming abrupt changes, or early warning signals, and provide a perspective on the contributions of palaeoclimate science to the understanding of abrupt changes in the Earth system. A synthesis of intervals of rapid climatic change evident in the geological record reveals some of the Earth system processes and tipping points that could lead to similar events in the future.
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