“…Mesoscale eddies are widely distributed in the global oceans, with the horizontal radius primarily ranging from 50 km to 300 km and vertical depths exceeding 1000 m (Chelton et al, 2011a;Dong et al, 2014;Zhang et al, 2014b;Li et al, 2024). They play crucial roles in the mid-to long-distance water mass exchange, material and energy transport, and vertical dynamic enhancement (Liu and Tang, 2018;Chen et al, 2023b). As one of the most complex regions in the ocean circulation system, the Northwest Pacific Ocean has a significant number of mesoscale eddies, exerting profound impacts on the distribution of temperature, salinity, and chlorophyll (Xu et al, 2016;Dong et al, 2017;Sun et al, 2022;Yuan and Hu, 2023).…”