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.
Cited by¶
1 citation across 1 artifact.
Each citation links to the sentence it supports in the citing article.
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.
Verification¶
Does it exist? Confirmed. This work's DOI resolves to a registered record, which fixes its identity. That is all it fixes.
Does it back the claim? Not recorded. The single citation of this work carries no recorded support check.
Support is checked per citation rather than per work — the same source can be cited soundly in one article and wrongly in another. Per-citation recording began recently, so a citation with no recorded check is a gap in the record rather than evidence it went unchecked.
See how references were verified.
Registry ID ref:9ab5e51f27ae · see in the full table