“…The first survey around the islands (K6 and K7) also showed higher densities in the immediate and eastern regions, especially in the lower epipelagic layer ( Figure 3b). As it is known that one of the branches of Oyashio, the western boundary current of the western subarctic gyre, reaches Sagami Bay or flows westward from the Izu Islands (Marumo, 1966;Sekine & Uchiyama, 2002;Senjyu, Asano, Matsuyama, & Ishimaru, 1998;Taira & Teramoto, 1985;Yang, Nagata, Taira, & Kawabe, 1993a, 1993b, the higher densities are attributed to the influence of Oyashio water. In the Kuroshio Extension area, the highest water density (lowest temperature and salinity) was shown north of the axis (Oyashio side) on the eastern side of…”