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| DC Field | Value | Language |
|---|---|---|
| dc.contributor.author | Patra, A K | - |
| dc.contributor.author | De, U K | - |
| dc.date.accessioned | 2016-09-21T11:11:01Z | - |
| dc.date.available | 2016-09-21T11:11:01Z | - |
| dc.date.issued | 1997-06 | - |
| dc.identifier.issn | 0975-105X (Online); 0367-8393 (Print) | - |
| dc.identifier.uri | http://nopr.niscair.res.in/handle/123456789/35491 | - |
| dc.description | 121-125 | en_US |
| dc.description.abstract | Occurrence of premonsoon thunderstorms striking DumDum, Calcutta, over a 12-year period has been studied based on a surface parameter (S) developed from surface observations at 0830 IST only. It has been found that on thunderstorm days the value of S in general lies between 1.00 and 1.60. It has also been found that 59.9% of premonsoon thunderstorms are of northerly type and 35.4% of southerly type. Nearly one-half of northerly developments are associated with wind squall, but in the case of southerly developments the wind squall association is only one-fifth. Southerly thunderstorms with wind squalls have almost a linear relationship between the parameter S and the time of occurrence. Moreover, south-easterly developments with squalls are more moist, have large wind speed of squall and occur early compared to the south-westerly developments with squalls. | 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(3) [June 1997] | en_US |
| dc.title | Role of a surface parameter on premonsoon thunderstorm days at DumDum (22.38°N, 88.28°E), Calcutta | en_US |
| dc.type | Article | en_US |
| Appears in Collections: | IJRSP Vol.26(3) [June 1997] | |
Files in This Item:
| File | Description | Size | Format | |
|---|---|---|---|---|
| IJRSP 26(3) 121-125.pdf | 274.12 kB | Adobe PDF | View/Open |
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