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Article
Relationship between vertical shear rate and kinetic energy dissipation rate in stably stratified flows
Geophysical Research Letters (2006)
  • Stephen de Bruyn Kops, University of Massachusetts - Amherst
  • D. A Hebert
Abstract
High resolution direct numerical simulations of strongly stratified turbulence are analyzed in order to investigate the relationship between vertical shearing of horizontal motions and the dissipation rate of kinetic energy. The relative magnitude of each component of the dissipation rate is examined as a function of the Reynolds number and of the buoyancy Reynolds number. From the simulation results, in conjunction with published laboratory results, it is concluded that (1) the simulation results are consistent with the laboratory data but span a much larger range of buoyancy Reynolds number, (2) the ratio of the square of the vertical shear rate to the dissipation rate is a strong function of buoyancy Reynolds number, and (3) the approximation that vertical shear rate is the dominant cause of energy dissipation rate is only good when the buoyancy Reynolds number is less than order one.
Publication Date
2006
Publisher Statement
Doi:10.1029/2005GL025071 An edited version of this paper was published by AGU. Copyright 2006 American Geophysical Union
Citation Information
Stephen de Bruyn Kops and D. A Hebert. "Relationship between vertical shear rate and kinetic energy dissipation rate in stably stratified flows" Geophysical Research Letters Vol. 33 (2006)
Available at: http://works.bepress.com/stephen_debruynkops/1/