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A series of zonal currents in the Pacific Ocean is investigated using eddy-permitting ocean general circulation models. The zonal currents in the subsurface are classified into two parts: one is a series of broad zonal flows that has the meridional pattern slanting poleward with increasing depth and the other is finescale zonal jets with the meridional scale of 3°-5°formed in each broad zonal flow. The basic pattern for the broad zonal flows is similar between the coarse-resolution model anddoi:10.1175/jpo2698.1 fatcat:564ynkgiwjg5zfbcnzrvaxtip4