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Northward near-surface Lagrangian transport of subtropical waters in theJapan Sea frontal zone is simulated and analysed based on altimeter data forthe period from 2 January 1993 to 15 June 2015. Computing differentLagrangian indicators for a large number of synthetic tracers launched weeklyfor 21 years in the southern part of the Sea, we find preferred transportpathways across the Subpolar Front. This cross-frontal transport isstatistically shown to be meridionally inhomogeneous with <q>gates</q> and<q>barriers</q> whose locations are determined by the local advection velocityfield. The gates <q>open</q> due to suitable dispositions of mesoscale eddiesfacilitating propagation of subtropical waters to the north. It is documentedfor the western, central and eastern gates with the help of different kindsof Lagrangian maps and verified by some tracks of available drifters. Thetransport through the gates occurs by a portion-like manner, i.e.subtropical tracers pass the gates in specific places and during specifictime intervals. There are some <q>forbidden</q> zones in the frontal area wherethe northward transport has not been observed during all the observationperiod. They exist due to long-term peculiarities of the advection velocityfield

Statistical analysis of Lagrangian transport of subtropical waters in the Japan Sea based on AVISO altimetry data