Symmetric instability under inertially resonant winds
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更新:2024-10-14 15:37:53 浏览:40次
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摘要
When wind aligns with the geostrophic flow in the upper ocean (down-front wind), it induces a negative Ertel potential vorticity (EPV) flux, initiating symmetric instability (SI) along the frontal boundary. However, surface mixed layers (SMLs) are usually subjected to fluctuating wind forcing rather than a constant, unidirectional one. Notably, near-inertial wind components can inject significant kinetic energy into the upper ocean, forming strong near-inertial oscillations. These variations in wind forcing, along with the associated near-inertial oscillations, introduce additional complexities to the energy budget of the SML. In this study, we investigate the frontal SI dynamics using large-eddy simulations with a series of wind conditions. A refined dynamical decomposition method is developed to achieve a more refined analysis of interaction between different motions. Using this method, we demonstrate that available potential energy (APE) also plays a crucial role in energizing SI. Furthermore, periodic winds enhance near-inertial motions within the system thereby rendering ageostrophic shear production (AGSP) a progressively dominant mechanism in the energy transfer process. Ultimately, our refined decomposition framework enables a detailed assessment of the feedback exerted by SI on the broader system dynamics.
关键词
surface mixed layer,symmetric instability,inertial gravity waves,large eddy simulation
稿件作者
Jialin Cao
Xiamen University
Lixin Qu
Shanghai Jiao Tong University
Bicheng Chen
Xiamen University
Zhiyu Liu
Xiamen University
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