即使在极端气候条件下,大西洋翻转循环仍在继续
J A Baker1, M J Bell2, L C Jackson2
1Met Office, Exeter, UK. jonathan.baker@metoffice.gov.uk.
Nature
|February 26, 2025
概括
大西洋南部翻转循环 (AMOC) 在本世纪不太可能崩. 南洋上升使AMOC稳定,即使在极端的气候变化场景下,防止崩.
科学领域:
- 气候科学
- 海洋学
- 地球系统科学
背景情况:
- 大西洋南部翻转循环 (AMOC) 对于全球热量分布至关重要.
- 由于全球变暖,预计AMOC的减弱引发了对气候影响的担忧.
- 关于AMOC减弱和潜在崩的程度存在不确定性.
研究的目的:
- 调查AMOC在极端气候强迫下的弹性.
- 通过温室气体和淡水变化来确定AMOC崩的可能性.
- 确定稳定AMOC的机制.
主要方法:
- 分析了34个模拟极端温室气体和北大西洋淡水强迫的气候模型.
- 对南大洋上游的研究及其对AMOC稳定性的影响.
- 评估太平洋南方翻转循环 (PMOC) 在弥补南洋上升的作用.
主要成果:
- 在所有34个气候模型中,AMOC表现出对极端强迫的适应性.
- 南大洋的上升持续维持了弱化的AMOC,防止了完全的崩.
- 虽然在大多数模型中出现了补偿PMOC,但它不足以完全平衡南洋上游.
结论:
- 由于稳定机制, AMOC在本世纪不太可能崩.
- 南洋和印度太平洋的循环是预测未来AMOC变化的关键因素.
- 了解这些循环对于预测对生态系统和海洋生物化学的影响至关重要.
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