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- W2604968444 abstract "M~s'aet Based on the current measurement data from the R/V Ryofu Maru of JMA in the equatorial area along 137E (1972---83) and 155E (1972--79) the structures of the zonal velocity of the Equatorial Undercurrent (EUC) and the North Equatorial Countercurrent (NECC) and their variations are systematically analyzed in detail. At 155~ the current at the equator and 100---300 m depth was a typical eastward EUC, it intensified in 1973--75, i.e., in the non-E[ Nino period. While the corresponding current at 137E was mostly westward, and the origin of the EUC shifted to north of the equator around 0.5~-1.5~ owing to the influence of the New Guinea Coast. The EUC origin disappeared in early July, 19~12. Comparing with the EUC disappearance at 159~ the average speed of an eastward travelling wave would be~l.ln~s. The velocity core of the NECC at 137E generally shifted northward in winter and southward in summer, and was stronger in summer and weaker in winter. The fluctuations of the I~ECC were closely related to those of the wind stress curl over the region 2--10~ 160~176" @default.
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- W2604968444 date "1986-01-01" @default.
- W2604968444 modified "2023-09-24" @default.
- W2604968444 title "CURRENT STRUCTURE AND ITS VARIATION EQUATORIAL AREA OF THE WESTERN NORTH PACIFIC OCEAN* IN THE" @default.
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