北大西洋亚热带模式水形成由海湾流前线控制
Bolan Gan1,2, Jingjie Yu1, Lixin Wu1,2
1Frontier Science Center for Deep Ocean Multispheres and Earth System (FDOMES) and Physical Oceanography Laboratory, Ocean University of China, Qingdao 266100, China.
National science review
|August 11, 2023
概括
面向尺度的海洋对大气的反显著影响北大西洋的亚热带模式水 (STMW) 形成. 准确地建模这种反对于理解海洋热量和碳吸收至关重要.
科学领域:
- 海洋学 海洋学 海洋学
- 气候科学 气候科学
- 大气科学 大气科学
背景情况:
- 亚热带模式水域 (STMWs) 是热量,碳和氧气的重要海洋储备.
- STMW形成发生在湾流地区,其特点是大气-海洋热面.
- 在STMW形成中,正面尺度海洋对大气 (FOA) 反的作用以前被低估了.
研究的目的:
- 用先进的气候模拟来研究FOA反对STMW形成的影响.
- 确定解决FOA反的必要性,以便在气候模型中准确地产生STMW.
主要方法:
- 利用了解决的全球气候模拟.
- 与没有抑制局部FOA反的模拟进行了比较.
- 评估FOA反对混合层深度,热损失和STMW特征的影响.
主要成果:
- 抑制局部FOA反将STMW的形成减少了近一半.
- FOA反通过混合层深化,由增加的潜在热量损失驱动,增强了STMW的突起.
- 与没有的模型相比,具有FOA反的形现象合模型更好地复制观察到的STMW.
结论:
- 对FOA反的准确表示对于改善气候模型中STMW形成至关重要.
- 仅仅提炼海洋分辨率是不够的,如果没有合的大气反.
- 地球系统模型必须纳入FOA反,以纠正低估的STMW和相关的生物地化学吸收.
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