Please use this identifier to cite or link to this item:
http://nopr.niscpr.res.in/handle/123456789/37671Full metadata record
| DC Field | Value | Language |
|---|---|---|
| dc.contributor.author | Kaushika, N. D. | - |
| dc.date.accessioned | 2016-11-28T05:09:55Z | - |
| dc.date.available | 2016-11-28T05:09:55Z | - |
| dc.date.issued | 1975-03 | - |
| dc.identifier.issn | 0975-105X (Online); 0367-8393 (Print) | - |
| dc.identifier.uri | http://nopr.niscair.res.in/handle/123456789/37671 | - |
| dc.description | 86-88 | en_US |
| dc.description.abstract | Medium scale TIDs in the equatorial anomaly region are investigated using the continuous records of electron content. TIDs are more intense during nighttime and often commence around sunrise and sunset times. It is suggested that sunrise heating and sunset cooling of the atmosphere could be the possible source of gravity waves causing these disturbances. | 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.04(1) [March 1975] | en_US |
| dc.title | TIDs in Equatorial Anomaly Region | en_US |
| dc.type | Article | en_US |
| Appears in Collections: | IJRSP Vol.04(1) [March 1975] | |
Files in This Item:
| File | Description | Size | Format | |
|---|---|---|---|---|
| IJRSP 4(1) 86-88.pdf | 377.77 kB | Adobe PDF | View/Open |
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