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Journal ArticleDOI

Collective instability of salt fingers

Melvin E. Stern
- 16 Jan 1969 - 
- Vol. 35, Iss: 02, pp 209-218
TLDR
In this article, the authors considered a steady laminar model of salt fingers and showed that the latter become unstable with respect to internal gravity waves when the finger Reynolds number exceeds a critical value.
Abstract
We first consider a steady laminar model of salt fingers and show that the latter become unstable with respect to internal gravity waves when the finger Reynolds number exceeds a critical value. The criterion is then used in speculations about the statistically steady state in a fully developed similarity model where horizontally averaged temperature and salinity gradients are constant at all depths. Dimensional reasoning is used to obtain the asymptotic dependence of the turbulent flux on the molecular salt diffusivity. From this and other relationships order-of-magnitude estimates are obtained and compared with laboratory experiments and ocean observations.

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Citations
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Journal ArticleDOI

Double-diffusive convection

TL;DR: In this paper, the authors present a rather personal view of the important developments in double-diffusive convection, a subject whose evolution has been the result of a close interaction between theoreticians, laboratory experimenters and sea-going oceano-graphers.
Journal ArticleDOI

The Contribution of Salt Fingers to Vertical Mixing in the North Atlantic Tracer Release Experiment

TL;DR: In this paper, the strength of salt-finger mixing has been diagnosed using a nondimensional parameter related to the ratio of the diffusivities for heat and buoyancy (Γ, “the dissipation ratio”).
Journal ArticleDOI

Compositional convection in a reactive crystalline mush and melt differentiation

TL;DR: In this paper, the authors describe experiments on the directional solidification of aqueous ammonium chloride solutions, where the addition of small amounts of a polymerizing agent permits variation of the solution viscosity independently of thermal conditions, phase diagram, and permeability.
Journal ArticleDOI

Transitional phenomena and the development of turbulence in stratified fluids: A review

TL;DR: In this paper, the authors focus on the transitional phenomena which precede, and may eventually lead to, the broadband spectra associated with turbulent flow, and apply this information to the natural environment (and emphasis is given to the oceans).
Journal ArticleDOI

A mechanism for layer formation in a double-diffusive fluid

TL;DR: In this article, the dynamics of layer formation by salt fingers from the uniform temperature and salinity gradients is studied by direct numerical simulations of the two-dimensional Navier-Stokes equations.
References
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Journal ArticleDOI

The “Salt-Fountain” and Thermohaline Convection

TL;DR: In this paper, the authors discuss the stability characteristic and the form of convective motion in the laminar regime of a convective model for vertical mixing of the sea and show that the model is unstable due to the fact that the molecular diffusivity of heat is much greater than the diffusivities of salt.
Journal ArticleDOI

Regularly spaced steps in the main thermocline near Bermuda

TL;DR: The main thermocline of the ocean off Bermuda is not a smooth gradient of temperature and salinity but consists of a remarkably regular series of steps of homogeneous layers 3 to 5 meters thick which alternate with transition layers 10 to 15 meters thick.