Please use this identifier to cite or link to this item: http://nopr.niscpr.res.in/handle/123456789/38006
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dc.contributor.authorLumb, H. M.-
dc.contributor.authorSetty, S. G. K.-
dc.date.accessioned2016-12-01T09:10:39Z-
dc.date.available2016-12-01T09:10:39Z-
dc.date.issued1973-12-
dc.identifier.issn0975-105X (Online); 0367-8393 (Print)-
dc.identifier.urihttp://nopr.niscair.res.in/handle/123456789/38006-
dc.description261-265en_US
dc.description.abstractThe time-dependent continuity equations for lour different ionic constituents (O+, O2+, N2+ NO+) together with the equations of motion for ions and neutral particles are solved numerically in the height range 120-800 km, The parameters for the various physical processes experienced by the plasma are taken into account in the calculations. A dynamic diffusion model of the neutral atmosphere has been taken. Results are presented for the winter temperature latitude (Delhi, geogr.lat., 28·5° N) ionosphere for low solar activity.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.02(4) [December 1973]en_US
dc.titleA Model F Layer at the Temperate Latitude Station, Delhien_US
dc.typeArticleen_US
Appears in Collections:IJRSP Vol.02(4) [December 1973]

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