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Direct numerical simulation of buoyancy-driven turbulence in stably stratified fluid

Published online by Cambridge University Press:  26 April 2006

Thomas Gerz  and
Hidekatsu Yamazaki
Thomas Gerz
Affiliation:
DLR, Institut für Physik der Atmosphäre W-8031 Oberpfaffenhofen, Germany
Hidekatsu Yamazaki
Affiliation:
Centre for Earth and Ocean Research, University of Victoria, PO Box 1700, Victoria, BC Canda, V8W 2Y2
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Abstract

We investigate the role of buoyancy force on the generation and decay of random motion in a homogeneously stratified fluid by means of direct numerical simulations (DNS) of the dynamic and thermodynamic equations. The simulations start from a fluid which is at rest but has appreciable temperature fluctuations. Therefore the flow initially evolves by extracting energy from the potential energy field. Three free parameters, the Reynolds number Re, the Prandtl number Pr and the stratification number St, characterize the flow. Among these numbers the stratification number, St = (lT0/T′0) (dTR/dz), is the most crucial one for the investigated problem. Here T′0 and lT0 are the initial r.m.s. temperature and the initial integral temperature lengthscale, respectively, and dTR/dz is the background stratification. St is a measure of the strength of background-temperature gradient compared to the initial mean fluctuating temperature gradient in the fluid.

A critical stratification number of order one is found to separate an oscillating, non-turbulent flow from flow states which exhibit features of turbulence. When St > 1, the statistics reveal a nearly linear and strongly anisotropic flow as typical for gravity waves but the flow-field variables behave randomly. When St < 1, i.e. when the initial gradient of fluctuating temperature exceeds the gradient of its background value, the available potential energy is sufficient to create nonlinear motions which resemble turbulence in many aspects. The properties of such a flow are a transient state of enhanced stirring and mixing, enhanced rates of dissipation of temperature fluctuations, and a quick return to isotropy.

The stratification number is an easily measurable parameter in field experiments in the ocean as well as in the atmosphere. Therefore St may be a useful indicator of whether a flow regime contains sufficient potential energy to create turbulence.

Type
Research Article
Information
Journal of Fluid Mechanics , Volume 249 , April 1993 , pp. 415 - 440
Copyright
© 1993 Cambridge University Press

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