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On the basis of the vertical distribution of 3H observed at the Geosecs station (1969) in the Northeast Pacific, the vertical eddy diffusivity in the thermocline was evaluated to be O.16cm2/sec. By using this value and dissolved oxygen profile, the consumption rate of oxygen in the thermocline was estimated to be 3.9 × 10-2 ml/kg/y on an average.

Vertical diffusivity and consumption rate of dissolved oxygen in the thermocline