Please use this identifier to cite or link to this item: http://nopr.niscpr.res.in/handle/123456789/38068
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dc.contributor.authorChakravarty, S. C.-
dc.contributor.authorRastogi, R. G.-
dc.date.accessioned2016-12-02T06:29:54Z-
dc.date.available2016-12-02T06:29:54Z-
dc.date.issued1972-06-
dc.identifier.issn0975-105X (Online); 0367-8393 (Print)-
dc.identifier.urihttp://nopr.niscair.res.in/handle/123456789/38068-
dc.description158-161en_US
dc.description.abstractLunar oscillation in the ionospheric absorption for the frequency 2•4 MHz at Kokubunji has been computed using the data for the period 1957-68. It has been found that the lunar tide in absorption at Kokubunji behaves in a way opposite to that of the tide at an equatorial station like Colombo. The phase of the tide during E-months shows a reversal compared to the other two seasons of the year. The amplitude of the tide increases with the increase of solar activity. The maximum amplitude of the lunar tide in absorption takes place at stations within 20ᵒ±5ᵒdip latitude.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.01(2) [June 1972]en_US
dc.titleLunar Effects in Ionospheric Absorption at Kokubunjien_US
dc.typeArticleen_US
Appears in Collections:IJRSP Vol.01(2) [June 1972]

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