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http://nopr.niscpr.res.in/handle/123456789/35642Full metadata record
| DC Field | Value | Language |
|---|---|---|
| dc.contributor.author | Datta, S | - |
| dc.contributor.author | Goswami, K | - |
| dc.contributor.author | De, U K | - |
| dc.date.accessioned | 2016-10-13T05:07:25Z | - |
| dc.date.available | 2016-10-13T05:07:25Z | - |
| dc.date.issued | 1996-04 | - |
| dc.identifier.issn | 0975-105X (Online); 0367-8393 (Print) | - |
| dc.identifier.uri | http://nopr.niscair.res.in/handle/123456789/35642 | - |
| dc.description | 79-81 | en_US |
| dc.description.abstract | During summer, the surface of ice deviates from its perfect crystalline structure. A concept of quasi-solid layer (QSL) is introduced. The depth of this QSL (hQSL) is estimated from a growth rate equation. The value of hQSL is found to be of the order of  m. A brief discussion is made of the results obtained under different atmospheric conditions. | 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.25(2) [April 1996] | en_US |
| dc.title | Depth of surface layer over ice during riming in supercooled atmosphere | en_US |
| dc.type | Article | en_US |
| Appears in Collections: | IJRSP Vol.25(2) [April 1996] | |
Files in This Item:
| File | Description | Size | Format | |
|---|---|---|---|---|
| IJRSP 25(2) 79-81.pdf | 210.91 kB | Adobe PDF | View/Open |
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