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°) 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 (EKE MS ) is relatively strong during spring–summer, whereas the submesoscale (50–150 km) EKE (EKE SM ) is significantly enhanced during winter–spring. The seasonal cycles of EKE MS and EKE SM are primarily controlled by the external forcing and BCI, respectively. In particular, the higher EKE MS 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 EKE SM seasonality and its contribution to the seasonally modulating EKE MS along the KC.