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http://nopr.niscpr.res.in/handle/123456789/37111Full metadata record
| DC Field | Value | Language |
|---|---|---|
| dc.contributor.author | Varkey, M J | - |
| dc.date.accessioned | 2016-11-17T04:32:00Z | - |
| dc.date.available | 2016-11-17T04:32:00Z | - |
| dc.date.issued | 1996-06 | - |
| dc.identifier.issn | 0975-1033 (Online); 0379-5136 (Print) | - |
| dc.identifier.uri | http://nopr.niscair.res.in/handle/123456789/37111 | - |
| dc.description | 160-162 | en_US |
| 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(-1)) is proportional to a process dependent vertical eddy mixing coefficient in water bodies away From surface, bottom and density discontinuities. | en_US |
| dc.language.iso | en_US | en_US |
| dc.publisher | NISCAIR-CSIR, India | en_US |
| dc.rights |  CC Attribution-Noncommercial-No Derivative Works 2.5 India | en_US |
| dc.source | IJMS Vol.25(2) [June 1996] | en_US |
| dc.title | Richardson Number, stability and turbulence - A coherent view | en_US |
| dc.type | Article | en_US |
| Appears in Collections: | IJMS Vol.25(2) [June 1996] | |
Files in This Item:
| File | Description | Size | Format | |
|---|---|---|---|---|
| IJMS 25(2) 160-162.pdf | 180.99 kB | Adobe PDF | View/Open |
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