Abstract
The new estimate of the average vertical mixing coefficient for the oceanic thermocline, based on all GEOSECS tritium data, is 1.7 ± 0.2 cm2 s-1.
Open access
The new estimate of the average vertical mixing coefficient for the oceanic thermocline, based on all GEOSECS tritium data, is 1.7 ± 0.2 cm2 s-1.
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