Tang, Tian, Zhang, Zhiwei, Zhang, Jinchao, Zhang, Xincheng, Sun, Zhongbin, and Feng, Zhe
The Kuroshio Loop Current (KLC) is an important form of Kuroshio intrusion into the northeastern South China Sea (NESCS), which has significant influences on dynamical and biogeochemical processes in the NESCS. Recent studies suggested that the KLC is a hot spot of submesoscale processes (submesoscales) with spatiotemporal scales of O(1–10) km and O(1–10) days, but submesoscales' roles in energy cascade and salt and heat transports remain obscure. Here, we investigate this issue through analyzing outputs from a 1/48° simulation. The kinetic energy exchange rate between submesoscale and larger‐scale processes (KER) is overall positive in the KLC region, which suggests the dominance of forward cascade. The magnitude of KER is comparable with the temporal change rate of larger‐scale kinetic energy in the upper 200 m. We also find that magnitude and direction of KER are closely associated with strain rate and horizontal divergence of background flows, respectively. In addition, the KLC region shows elevated submesoscale salinity and heat diffusivities with magnitudes reaching O(102) m2 s−1. During the KLC period, horizontal mixing by submesoscales can transport 0.90 × 1013 kg salt and 0.71 × 1020 J heat westward into the NESCS interior, which are an order of magnitude larger than those caused by the mesoscale eddy shedding from the KLC. These results suggest that submesoscales play important roles not only in energy cascade but also in salt and heat transports in the KLC region. Therefore, the roles of submesoscales should be taken into account when studying energy, salt, and heat budgets in the NESCS. Plain Language Summary: As the western boundary current of the North Pacific subtropical gyre, the Kuroshio can intrude into the northeastern South China Sea (NESCS) in the form of Kuroshio Loop Current (KLC), which modulate the tracer and energy budgets of NESCS through shedding eddies. Although previous studies have reported that the KLC region is abundant with submesoscale processes (submesoscales) with spatiotemporal scales of O(1–10) km and O(1–10) days, their roles in cross‐scale energy transfer and salt and heat transports are poorly known. Here, the above issues are examined through an analysis of outputs from a 1/48° ocean simulation. We find that larger‐scale processes generally feed submesoscales through a forward energy transfer in upper 200 m, whose rate is comparable in magnitude with the temporal change rate of larger‐scale kinetic energy. Furthermore, the horizontal mixing effect of submesoscales can transport a huge amount of heat and salt westward into the NESCS interior during the KLC period. The salt and heat transports are an order of magnitude larger than those caused by the mesoscale eddy shedding from the KLC. The above results suggest that submesoscales associated with the KLC play important roles in the energy, heat, and salt budgets in the NESCS. Key Points: Submesoscales in the Kuroshio Loop Current (KLC) are examined using high‐resolution simulation outputsEnergy exchange between submesoscales and KLC plays an important role in the local energy budgetHorizontal salt and heat transports by submesoscales are much larger than those by mesoscale eddy shedding from the KLC [ABSTRACT FROM AUTHOR]