A One-Dimensional Model of the Seasonal Thermocline II. The General Theory and Its Consequences.¶
Kraus, E. B., & Turner, J. S. (1967). A One-Dimensional Model of the Seasonal Thermocline II. The General Theory and Its Consequences. Tellus, 19(1), 98-106.
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Primes¶
- Mixed Layer
- Oceanography (origin) — the upper-ocean mixed layer is wind- and wave-stirred, locally uniform in temperature and salinity, capped below by the thermocline; it mediates all atmosphere-ocean exchange of heat, gas, and momentum, and its depth gates the nutrient flux that controls primary productivity.
This sourceFoundational mixed-layer model: wind- and wave-driven turbulent mixing produces a vertically uniform surface layer over a sharp thermocline, with layer depth governed by a turbulent-kinetic-energy budget.
- Oceanography (origin) — the upper-ocean mixed layer is wind- and wave-stirred, locally uniform in temperature and salinity, capped below by the thermocline; it mediates all atmosphere-ocean exchange of heat, gas, and momentum, and its depth gates the nutrient flux that controls primary productivity.
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