dc.contributor.author | Varkey, M.J. | |
dc.date.accessioned | 2009-01-21T11:25:30Z | |
dc.date.available | 2009-01-21T11:25:30Z | |
dc.date.issued | 1996 | |
dc.identifier.citation | Indian Journal of Marine Sciences, Vol.25; 160-162p. | |
dc.identifier.uri | http://drs.nio.org/drs/handle/2264/2281 | |
dc.description.abstract | As 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.iso | en | |
dc.publisher | NISCAIR, CSIR | |
dc.rights | Copyright [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.subject | turbulence | |
dc.subject | stability | |
dc.subject | richardson number | |
dc.title | Richardson Number, stability and turbulence- A coherent view | |
dc.type | Journal Article | |