“…The initial and side boundary conditions for the ROMS were provided by monthly climatology of the assimilative JCOPE2 oceanic reanalysis (Miyazawa et al, 2009). A one-way offline nesting technique was employed to convey the parent JCOPE2 to the child ROMS model with grid resolution refinement (e.g., Mason et al, 2010;Uchiyama et al, 2014;Kamidaira et al, 2017;Uchiyama et al, 2017;Kamidaira et al, 2018;Uchiyama et al, 2018a;Uchiyama et al, 2018b;Uchiyama et al, 2018c;Tada et al, 2018;Masunaga et al, 2018;Kamidaira et al, 2019;Masunaga et al, 2019;Zhang et al, 2019;Kurosawa et al, 2020;Kamidaira et al, 2021;Takeda et al, 2021;Uchiyama et al, 2022;Masunaga et al, 2022;Matsushita et al, 2022). Therefore, the horizontal grid spacing was successfully reduced from 1/12°(~10 km) of the JCOPE2 reanalysis to 3 km of the ROMS model, and vertically into stretched 32 s-layers (Shchepetkin and McWilliams, 2005) with grid height refinement near the surface and bottom to adequately resolve the boundary layers.…”