Seasonal Variability of Eddy Kinetic Energy along the Kuroshio Current

The seasonal variability of the eddy kinetic energy (EKE) along the Kuroshio Current (KC) is examined using outputs from an eddy-resolving (1/10 & DEG;) ocean model. Using a theoretical framework for climatological monthly mean EKE, the mechanisms governing the seasonal cycle of upper-ocean EKE are investigated. East of Taiwan, the EKE shows two comparable peaks in spring and summer in the surface layer; only the spring one is evident in the subsurface layer. The seasonality is determined by mixed barotropic (BTI) and baroclinic (BCI) instabilities. Northeast of Taiwan, the EKE is also elevated during spring-summer but with a sole peak in summer, which is dominated by the meridional EKE advection by the KC. In the middle part of the KC in the East China Sea, the mesoscale (.150 km) EKE (EKEMS) is relatively strong during spring-summer, whereas the submesoscale (50-150 km) EKE (EKESM) is significantly enhanced during winter-spring. The seasonal cycles of EKEMS and EKESM are primarily controlled by the external forcing and BCI, respectively. In particular, the higher EKEMS level in summer is mainly due to the increased wind work. West of the Tokara Strait, the EKE exhibits a prominent peak in winter and has its minimum in summer, which is regulated by the BCI. As the submesoscale signals are partially resolved by the model, further studies with higher-resolution simulations and observations are needed for a better understanding of the EKESM seasonality and its contribution to the seasonally modulating EKEMS along the KC.

Automated summary

The study investigates the seasonal variability of the eddy kinetic energy (EKE) along the Kuroshio Current (KC) using outputs from an eddy-resolving ocean model. It reveals that the seasonal cycle of EKE is determined by the interaction of large-scale and small-scale instabilities. The EKE exhibits different patterns and mechanisms in different regions of the KC, with factors such as advection, external forcing, and baroclinic and barotropic instabilities playing a role.