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dc.contributor.authorVarkey, M.J.
dc.date.accessioned2009-01-21T11:25:30Z
dc.date.available2009-01-21T11:25:30Z
dc.date.issued1996
dc.identifier.citationIndian Journal of Marine Sciences, Vol.25; 160-162p.
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/2281
dc.description.abstractAs turbulence in water is governed by vertical mobility controlled by static stability and horizontal mobility controlled by currents, the Richardson Number should give a measure of turbulence also. It is argued in this note that inverse of the Richardson Number (Ri sup(-1)) is proportional to a process dependent vertical eddy mixing coefficient in water bodies away from surface, bottom and density discontinuities.
dc.language.isoen
dc.publisherNISCAIR, CSIR
dc.rightsCopyright [1996]. All efforts have been made to respect the copyright to the best of our knowledge. Inadvertent omissions, if brought to our notice, stand for correction and withdrawal of document from this repository.
dc.subjectturbulence
dc.subjectstability
dc.subjectrichardson number
dc.titleRichardson Number, stability and turbulence- A coherent view
dc.typeJournal Article


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