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深北冰洋的变暖是由从大西洋深处转移的热量增强的
Ruizhe Song1,2,3,4, Xianyao Chen1,2,3, Hanwen Bi1,2,3,4
1Frontier Science Center for Deep Ocean Multispheres and Earth System, Ocean University of China, Qingdao, China.
Science advances
|November 19, 2025
概括
北极大洋的深水正在由于气候变化而迅速变暖,而不仅仅是地热加热. 这种变暖对欧亚盆地产生影响,而美洲盆地由于地理障碍而保持较冷.
科学领域:
- 海洋学 海洋学 海洋学
- 气候科学 气候科学
- 北极研究 北极研究
背景情况:
- 自20世纪90年代以来,在北冰洋深处和底部观察到广泛的变暖.
- 从历史上看,对北极深度变暖的归因主要集中在地热加热上.
- 全球和北极气候变化对深海变暖的影响尚不清楚.
研究的目的:
- 为了调查北冰洋深度和底部变暖的驱动因素.
- 量化特定北极盆地的变暖速度.
- 为了确定气候变化对北冰洋深层温度的影响.
主要方法:
- 从20世纪90年代开始对观测数据的分析.
- 在2000至2600米之间的欧亚盆地温度测量.
- 模拟海洋流和地理特征 (弗拉姆海峡,洛莫诺索夫山脊) 对热量分布的影响.
主要成果:
- 欧亚盆地的深北冰洋水正在每十年升温0.020°C,超过地热加热.
- 格陵兰深盆地的变暖减少了通过弗拉姆海峡对欧亚盆地的冷却效应.
- 洛莫诺索夫山脊阻碍了变暖信号的传播,导致深美洲亚洲盆地变暖速度减缓 (0.003°C/十年).
结论:
- 气候变化,特别是格陵兰盆地深层地区的变暖,是北冰洋深层地区变暖的重要驱动因素.
- 地热加热本身无法解释观察到的变暖速度.
- 深格陵兰盆地变暖对更广泛的深北冰洋生态系统有明显的影响.
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