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dc.contributor.authorDavid, T. W-
dc.contributor.authorAyoade, A. O-
dc.date.accessioned2022-07-19T10:53:59Z-
dc.date.available2022-07-19T10:53:59Z-
dc.date.issued2008-
dc.identifier.citationDavid, T. W. & Ayoade, A. O. (2008). RESPONSE OF THE IONOSPHERE TO INTENSE GEOMAGNETIC STORM. International Journal of Natural and Applied Sciences, 4(1): 86-91MSen_US
dc.identifier.urihttp://localhost:8080/xmlui/handle/123456789/789-
dc.description.abstractRecent results of the study of intense geomagnetic storms show that the depletion of f0F2 was simultaneously worldwide and extended to very low latitudes. In this light, this work investigates the nature of ionospheric response associated with another intense geomagnetic storm of July 13- 14, 1982. The investigation used measured parameters of solar wind plasma and imbedded IMF, and f0F2 data obtained from a global network of ionosondes. The analyses of the results show that contrary to the opinion that intense storm causes depletion in the upper latitude, the upper latitude of Argentine Island showed an intense positive storm (enhancement). In addition, the depletion down the latitude is irregular and also lacked simultaneityen_US
dc.description.sponsorshipT. W. David and A. O. Ayoadeen_US
dc.language.isoenen_US
dc.publisherInternational Journal of Natural and Applied Sciencesen_US
dc.relation.ispartofseries4;1-
dc.subject: Geomagnetic storms, solar wind plasma, magnetosphere, ionosphereen_US
dc.titleRESPONSE OF THE IONOSPHERE TO INTENSE GEOMAGNETIC STORMSen_US
dc.typeArticleen_US
Appears in Collections:Physics

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