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Wind-produced horizontal circulation in the Pacific, considered as zonal motion, in the presence of both vertical and horizontal eddy viscosity
Hidaka, K. (1972). Wind-produced horizontal circulation in the Pacific, considered as zonal motion, in the presence of both vertical and horizontal eddy viscosity, in: Takenouti, A.Y. (Ed.) Biological oceanography of the north Pacific Ocean. pp. 83-95
In: Takenouti, A.Y. (Ed.) (1972). Biological oceanography of the north Pacific Ocean. Idemitsu Shoten: Tokyo. , meer
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  • Hidaka, K.
Abstract
    Wind-produced steady horizontal motion of water in the Pacific Ocean was computed assuming the measured wind stress distribution and disregarding the wind-produced slope of the sea surface. It was concluded from numerical computations that wind-produced current vectors deviate 45°s cum sole from the direction of the wind stress, except at and close (within less than 1° 5N and S) to the equator. A spiral similar to Ekman's was obtained for several different combinations of both horizontal and vertical eddy viscosity.
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