tipping级联旁的稳定作用：AMOC-冰冻圈系统
A place for stabilization alongside tipping cascades: the AMOC-cryosphere system
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中文总结 AI 辅助
本文聚焦AMOC-冰冻圈系统，指出二者相互作用可抑制级联转变，提出需从关注稳定与去稳定动态、构建适配框架及开发相关方法三方面完善临界点风险评估。
中文摘要 AI 辅助
大西洋经向翻转环流（AMOC）与冰冻圈是临界点研究的核心对象，二者的相互作用通常被视为级联转变的路径。本文综述了相关证据，表明这些相互作用也可抑制变化，影响其幅度与时间，甚至在某些情况下决定转变是否发生。作者认为，要更全面评估临界点风险，需在三个方面取得进展：系统关注稳定与去稳定动态并存的情况；构建能容纳竞争性及依赖情境效应的概念框架；开发检测、预测与归因稳定作用的方法。
英文摘要
The Atlantic Meridional Overturning Circulation (AMOC) and cryosphere are central to tipping-point research, where their interactions are typically framed as pathways for cascading transitions. Here, I review evidence that these interactions can also oppose change, affecting its magnitude and timing or, in some cases, whether a transition occurs at all. I argue that a more complete assessment of tipping risk requires progress on three fronts: systematic attention to stabilizing alongside destabilizing dynamics, conceptual frameworks that accommodate competing and context-dependent effects, and methods to detect, anticipate, and attribute stabilization.
