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在海洋中常见的地表热浪和冷浪
Qingyou He1,2, Weikang Zhan1,2, Ming Feng3
1State Key Laboratory of Tropical Oceanography, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou, China.
Nature
|October 16, 2024
概括
海底极端温度, 像海洋热浪和寒流, 往往是由海洋旋驱动的, 而不是表面事件. 这些带来的极端现象正在加剧,
科学领域:
- 海洋学
- 气候科学
- 海洋生物学
背景情况:
- 由于全球变暖,包括海洋热浪 (MHW) 和海洋寒冷 (MCS) 在内的极端海洋温度事件正在增加.
- 研究的重点是表面事件, 留下了地下海洋极端及其驱动因素.
- 地下海洋是大部分海洋生物的所在地,对于了解气候影响至关重要.
研究的目的:
- 调查中等层次旋在地下海洋热浪和寒流中的作用.
- 在海洋表面下确定极端温度事件的驱动因素.
- 评估海底极端温度事件的强化趋势
主要方法:
- 使用全球观测数据分析海底极端温度.
- 将地表MHW和MCS与地表事件进行比较,并将它们与中层层相对应.
- 检查了反旋风和旋风中地下MHW和MCS的发生情况.
主要成果:
- 80%的地下MHW和MCS (100米以下) 与地表事件无关.
- 中级旋流对地下MHW和MCS产生重大影响,特别是在亚热带旋流和主流系统中.
- 连接到旋的地表温度极端变得比海洋背景温度更快.
结论:
- 中等层次的旋是地下极端海洋温度事件的关键驱动因素.
- 地表MHW和MCS通常与地表事件脱而出.
- 随着全球变暖, 海洋旋对地表极端温度的影响也在增加.
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