Abstract The North Pacific Intermediate Water (NPIW) originates as a vertical salinity minimum in the mixed water region (MWR) between the Kuroshio and Oyashio, just east of Japan. Salinity minima in this region are examined and related to the water man structures, dynamical features, and winter mixed layer density of waters of Oyashio origin. Stations in the MWR are divided into five regimes, of which three represent source waters (from the Kuroshio, Oyashio, and Tsugaru Current) and two are mixed waters formed from these three inputs. Examination of NPIW at stations just east of the MWR indicates that the mixed waters in the MWR are the origin of the newest NPIW. Multiple salinity minima with much finestructure are seen throughout the MWR in spring 1989, with the most fragmented occurring around the large warm core ring centered at 37°N, 144°E, suggesting that this is a dominant site for salinity minimum formation. The density of the NPIW in the MWR is slightly higher than the apparent late winter surfa...
CITATION STYLE
Talley, L. D., Nagata, Y., Fujimura, M., Iwao, T., Kono, T., Inagake, D., … Okuda, K. (1995). North Pacific Intermediate Water in the Kuroshio/Oyashio Mixed Water Region. Journal of Physical Oceanography, 25(4), 475–501. https://doi.org/10.1175/1520-0485(1995)025<0475:npiwit>2.0.co;2
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