Interannual variability in the baroclinic gyre structure of the western North Pacific from 1954-1974
In the western North Pacific from 0-35N 130-180E, the vertical and horizontal thermal structure of the baroclinic gyre systems in the region from 0-400 m depth has been mapped on a yearly basis from 1954-1974. From this measure of the baroclinic field of mass, the dynamic height (0/400 db) has been computed for each year, yielding geostrophic current indices of the major zonal currents....
White, Warren B., and Keiichi Hasunuma. 1980. "Interannual variability in the baroclinic gyre structure of the western North Pacific from 1954-1974." Journal of Marine Research 38, (4). https://elischolar.library.yale.edu/journal_of_marine_research/1523