The formation of a layered structure when a stable salinity gradient is heated from below
- 1 September 1987
- journal article
- research article
- Published by Cambridge University Press (CUP) in Journal of Fluid Mechanics
- Vol. 182 (-1), 525-541
- https://doi.org/10.1017/s0022112087002441
Abstract
It is well known that heating a stable salinity gradient from below leads to the formation of a series of turbulently convecting layers separated by stable diffusive interfaces. It is argued theoretically and demonstrated experimentally that the first mixed layer grows to a critical height δc, which is determined by a balance between the vertical kinetic and potential energies of the turbulent eddies, before a growing second layer separated from the first layer by a quasi-stationary stable density interface can be formed. Although the thermal boundary layer that develops over the propagating turbulent front can become unstable and form a second mixed region before the first layer grows to δc, the density interface formed between these two layers is not sufficiently stable to resist quick entrainment of the second layer into the lower layer. Some aspects of the growth of the first turbulent layer and possible application of the results to oceanic situations are also discussed.Keywords
This publication has 24 references indexed in Scilit:
- On Heat Transfer Through the Ocean FloorPublished by Wiley ,2013
- Laboratory studies of the entrainment zone of a convectively mixed layerJournal of Fluid Mechanics, 1980
- On heating a stable salinity gradient from belowJournal of Fluid Mechanics, 1979
- A theory of mixing in a stably stratified fluidJournal of Fluid Mechanics, 1978
- The deepening of a mixed layer in a stratified fluidJournal of Fluid Mechanics, 1975
- The structure of turbulent density interfacesJournal of Fluid Mechanics, 1974
- Stability of thermal convection in a salinity gradient due to lateral heatingInternational Journal of Heat and Mass Transfer, 1971
- Measurements of temperature and electrical conductivity in Lake Vanda, Victoria Land, AntarcticaNew Zealand Journal of Geology and Geophysics, 1968
- The effect of heating rate on the stability of stationary fluidsJournal of Fluid Mechanics, 1967
- Visual Detection of Temperature-Density Discontinuities in Water by DivingScience, 1955