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- W1417000462 abstract "Publisher Summary This chapter discusses several aspects of fluid dynamics that are useful in understanding and modifying the density structure in saline lakes. Small and strongly stratified lakes possess small rates of vertical mixing; thus, their vertical density structure could be easily altered and controlled. In fluids stratified by temperature and salinity, the qualitative nature of the convection and mixing can be different from those that occur in either pure thermal or pure haline convection. This is called “Double Diffusive” convection. The difference between the diffusivity of heat and salt (at the molecular level) is the underlying cause of a hierarchy of large-scale motions that are produced in a fluid whose mean density field decreases upwards. Surface cooling can result in significant cooling of the bottom water without destructing the pycnocline. The surface cooling can be achieved by the double-diffusive mechanics that allow the potential energy associated with the temperature field to be released without destructing the pycnocline." @default.
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- W1417000462 date "1980-01-01" @default.
- W1417000462 modified "2023-09-24" @default.
- W1417000462 title "Chapter 2 Mixing in Stratified Fluids" @default.
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- W1417000462 doi "https://doi.org/10.1016/s0070-4571(08)70226-7" @default.
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