Please use this identifier to cite or link to this item: http://nopr.niscpr.res.in/handle/123456789/36218
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dc.contributor.authorMahajan, K K-
dc.date.accessioned2016-10-26T07:38:20Z-
dc.date.available2016-10-26T07:38:20Z-
dc.date.issued1991-10-
dc.identifier.issn0975-105X (Online); 0367-8393 (Print)-
dc.identifier.urihttp://nopr.niscair.res.in/handle/123456789/36218-
dc.description388-395en_US
dc.description.abstractA powerful transmitter and a large transmitting-receiving antenna are the basic requirements of an incoherent scatter radar. The system specifications of the Indian MST radar located at Gadanki (13.5°N, 79°E) with peak power-aperture product of about 3 x 1010 Wm2 meet these requirements. Although the operating frequency of 53 MHz is not ideal for incoherent scatter sounding (due to very large sky background noise at this frequency), the signal can be usefully processed to obtain some basic ionospheric parameters like electron density, electron temperature, ion temperature, ion composition, ion drifts and E-region collision frequency. This radar, being located a little away from the electrojet, will also be able to make measurements for heights below 200 km, where the Jicamarca radar cannot. An immediate contribution in the incoherent scatter mode would be electron density measurements in the E-F valley for which no information is available for an equatorial station. Further, the radar would also prove useful for studies of equatorial spread-F, winds and waves in the thermosphere and equatorial anomaly.en_US
dc.language.isoen_USen_US
dc.publisherNISCAIR-CSIR, Indiaen_US
dc.rights CC Attribution-Noncommercial-No Derivative Works 2.5 Indiaen_US
dc.sourceIJRSP Vol.20(5) [October 1991]en_US
dc.titleAdding incoherent scatter mode to the Indian MST radar for upper atmospheric studiesen_US
dc.typeArticleen_US
Appears in Collections:IJRSP Vol.20(5) [October 1991]

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