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http://nopr.niscpr.res.in/handle/123456789/35535Full metadata record
| DC Field | Value | Language |
|---|---|---|
| dc.contributor.author | Chanda, A | - |
| dc.contributor.author | De, A K | - |
| dc.contributor.author | Das, J | - |
| dc.date.accessioned | 2016-10-04T09:47:59Z | - |
| dc.date.available | 2016-10-04T09:47:59Z | - |
| dc.date.issued | 1997-12 | - |
| dc.identifier.issn | 0975-105X (Online); 0367-8393 (Print) | - |
| dc.identifier.uri | http://nopr.niscair.res.in/handle/123456789/35535 | - |
| dc.description | 307-311 | en_US |
| dc.description.abstract | The fractal technique, as developed and applied by Grassberger [Nature (UK), 323 (1986) 609] for atmospheric variables, has been used for interpretation of velocity field data near ground during the early monsoon period. It has generally been observed that while both the horizontal components of wind possess low dimensional strange attractors, in the case of the vertical velocity field there is practically no evidence of strange attractor. An explanation of this anomalous behaviour of the vertical velocity field has been provided. | 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 | IJRSP Vol.26(6) [December 1997] | en_US |
| dc.title | On the fractal characterisation of atmospheric velocity field | en_US |
| dc.type | Article | en_US |
| Appears in Collections: | IJRSP Vol.26(6) [December 1997] | |
Files in This Item:
| File | Description | Size | Format | |
|---|---|---|---|---|
| IJRSP 26(6) 307-311.pdf | 372.51 kB | Adobe PDF | View/Open |
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