基于物理的早期预警信号显示,AMOC正在改变方向
René M van Westen1, Michael Kliphuis1, Henk A Dijkstra1
1Institute for Marine and Atmospheric Research Utrecht, Utrecht University, Princetonplein 5, Utrecht 3584 CC, Netherlands.
Science advances
|February 9, 2024
概括
大西洋南部翻转循环 (AMOC) 可能因淡水输入而崩. 一个新的早期预警信号,即最低淡水运输,预测了AMOC倾斜事件,并表明当前系统正在接近这一关键值.
科学领域:
- 气候科学是气候科学.
- 海洋学 海洋学 海洋学
- 地球系统建模模型
背景情况:
- 大西洋南部翻转循环 (AMOC) 是一个关键的气候倾斜元素.
- 北大西洋的淡水输入构成AMOC崩的风险.
- 之前的研究在模型中诱导了AMOC崩,但没有研究倾斜事件过程.
研究的目的:
- 调查AMOC倾斜事件的过程和影响.
- 开发一个基于物理的和可观察的AMOC倾斜早期预警信号.
- 评估AMOC与倾倒有关的当前状态.
主要方法:
- 使用社区地球系统模型模拟了一个AMOC倾斜事件.
- 分析了与AMOC崩相关的气候影响.
- 在大西洋南部边界开发了基于淡水运输的早期预警信号.
- 评估了经典的统计早期预警信号.
主要成果:
- 这项研究首次对AMOC倾斜事件及其显著气候影响进行了模拟.
- 开发了一种新的早期预警信号,即最小的AMOC诱导的淡水运输.
- 重新分析的数据表明,当今的AMOC正在接近一个临界点.
- 经典的统计早期预警信号被发现对分析的时间间隔敏感.
结论:
- 开发的早期预警信号为传统方法提供了基于物理的可观测替代方案.
- 这些发现表明,AMOC目前正朝着潜在的倾斜方向发展.
- 了解AMOC倾斜动态对于预测未来气候变化影响至关重要.
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