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- W66651858 abstract "Abstract A two-layer thermocline model driven in the upper layer by heating and wind mixing and in the lower layer by mixing, caused by turbulence from a bottom current, is investigated. It is found that the turbulence in the lower layer may force the thermocline towards the sea surface and thereby decrease the temperature difference between the layers as compared to the case without mixing in the lower layer. Under such circumstances there will be an exchange of water through the thermocline, caused by entrainment from both sides of the thermocline. When occurring this may have a great importance for the biological plant production as nutrients from below are perpetually supplied to the upper layer despite the existence of the thermocline. The two-layer stratification breaks down and a shelf front is created where a length formed by the wind speed, the current speed and the buoyancy flux is equal to the local water depth. This later result is in accordance with the result of Simpson, Allen and Morris (1978)." @default.
- W66651858 created "2016-06-24" @default.
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- W66651858 date "1981-01-01" @default.
- W66651858 modified "2023-10-05" @default.
- W66651858 title "Cross Thermocline Flow on Continental Shelves and the Locations of Shelf Fronts." @default.
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- W66651858 doi "https://doi.org/10.1016/s0422-9894(08)70403-3" @default.
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