T. Gamo et al., Recent upward shift of the deep convection system in the Japan Sea, as inferred from the geochemical tracers tritium, oxygen, and nutrients, GEOPHYS R L, 28(21), 2001, pp. 4143-4146
The thermohaline circulation system in the Japan Sea, an almost land-lock-e
d marginal sea in the northwest Pacific, is now in a transition state. Comp
arison of vertical profiles of tritium, oxygen and nutrients between 1984 a
nd 1998 demonstrates the following Mo points: (1) the supply of dense surfa
ce seawater to the bottom layer (>2,500 in in depth) has almost ceased sinc
e 1984, and (2) the intrusion of surface seawater to an intermediate depth
range (between similar to 700 in and similar to2,000 m in depth) has been r
einforced during this 14-year period. Such transitional upward shift of the
thermohaline conveyor belt in the Japan Sea is thought to have separated t
he bottom water from the conveyor belt and brought about a stagnant mode of
the bottom water.