人类引起的海面温度强化的季节性周期
Fukai Liu1, Fengfei Song2,3, Yiyong Luo4
1Frontiers Science Center for Deep Ocean Multispheres and Earth System and Physical Oceanography Laboratory, Ocean University of China, Qingdao, China. fliu@ouc.edu.cn.
Nature communications
|May 10, 2024
概括
海洋的海洋海洋的海洋.
科学领域:
- 海洋学 海洋学 海洋学
- 气候科学 气候科学
- 环境科学 环境科学
背景情况:
- 海面温度 (SST) 季节性周期对生态系统和社会产生影响.
- 以前的研究表明,由于全球变暖,SST周期加剧.
- 这些变化的历史证据仍然不清楚.
研究的目的:
- 为了确定SST季节周期是否在历史记录中加剧.
- 量化SST季节性的全球和区域变化.
- 为了确定所观察到的SST季节性周期强化背后的驱动因素.
主要方法:
- 对1983-2022年全球海面温度数据的分析.
- 归因研究以确定SST季节性变化的驱动因素.
- 研究混合层深度和表面热流变化的研究.
主要成果:
- 从1983年到2022年,全球SST季节周期的加剧率为3.9%±1.6%.
- 热点,如北极次极旋转,显示高达10%的强化.
- 增加的温室气体和减少的气溶被确定为主要驱动因素.
结论:
- 近几十年来,SST季节周期的加剧显而易见.
- 人为排放的变化,影响混合层深度,是关键驱动因素.
- 加剧的SST季节性影响上层海洋氧化和海洋生态系统.
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