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Turbulent vertical kinetic energy in the ocean mixed layer

ABSTRACT

Vertical velocities in the ocean boundary layer were measured for two weeks at an open ocean, wintertime site using neutrally buoyant floats. Simultaneous measurements of the surface meteorology and surface waves showed a large variability in both wind and wave properties and only weak correlations between them. Buoyancy forcing was weak. The mean square vertical velocity in the boundary layer (sigma)^sup 2^^sub w^ measured from the vertical motion of the floats was proportional to the squared friction velocity u^sup 2^^sub *^ estimated from shipboard meteorological measurements using bulk formulas. Thus (sigma)^sup 2^ = A(overscored)u^sup 2^^sub *^ (the rate of momentum transport ...

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