北大西洋多个世纪的内部变化可能会在欧洲带来额外的变暖
A Al-Yaari1,2, D Swingedouw3, P Braconnot4
1Univ. Bordeaux, CNRS, Bordeaux INP, EPOC, UMR 5805, F-33600, Pessac, France. amen.al.yaari@vub.be.
Nature communications
|February 10, 2026
概括
北大西洋的内部变化显著影响欧洲的温度. 这项研究证实了这种多世纪模式,与大西洋南部翻转循环有关,解释了最近的放大变暖.
科学领域:
- 气候科学 气候科学
- 古气候学 古气候学
- 海洋学 海洋学 海洋学
背景情况:
- 近几十年来,欧洲经历了显著的变暖.
- 北大西洋多个世纪的内部变化被假定会影响欧洲的温度.
- 在此之前,有限的高分辨率代理数据阻碍了观察性评估.
研究的目的:
- 证明北大西洋多个世纪内部变化的存在和幅度的量化.
- 评估这种变化对欧洲温度的影响.
- 将这种变化与大西洋南部翻转循环联系起来.
主要方法:
- 一年到十年的基于Proxy的Holocene重建的汇编.
- 仪器观测的整合.
- 对气候模型模拟的分析.
主要成果:
- 证明了北大西洋多个世纪的变化模式的存在.
- 量化了这种可变性模式的幅度.
- 建立了这种模式与大西洋南部翻转循环的内部变化之间强烈的联系.
- 表明这种模式解释了20世纪温度变化的部分原因.
- 确定了20世纪90年代末进入积极阶段的转变,有助于放大最近欧洲的变暖.
- 量化表明,这种内部变异性可能会在2000-2035年期间在北欧增加高达30%的人为变暖.
结论:
- 多个世纪的内部变化模式显著影响欧洲的气候.
- 大西洋南部翻转循环的变化是这种模式的关键驱动因素.
- 这种自然变异性在调节欧洲人为变暖趋势方面发挥着至关重要的作用.
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