On the Upper-Ocean Vertical Eddy Heat Transport in the Kuroshio Extension. Part I: Variability and Dynamics
On the Upper-Ocean Vertical Eddy Heat Transport in the Kuroshio Extension. Part I: Variability and Dynamics
复制标题
黑潮延伸部分的上层海洋垂直涡流热传输。
DOI：
10.1175/jpo-d-20-0068.1
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发表时间：
2020-11
影响因子：
3.5
通讯作者：
ran
中科院分区：
文献类型：
--
作者：
Peiran Yang;Zhao Jing;Bingrong Sun;Lixin Wu;Bo Qiu;Ping Chang;Sanjiv Ramach;ran
海洋涡旋在将热量从次表层输送到表层海洋中起着至关重要的作用。然而，垂直涡动热输送QT的动力机制还没有得到系统的研究，特别是在西边界混合层中
Oceanic eddies play a crucial role in transporting heat from the subsurface to surface ocean. However, dynamics responsible for the vertical eddy heat transport QT have not been systematically understood, especially in the mixed layer of western boundary