RESPONSE OF THE IONOSPHERE TO INTENSE GEOMAGNETIC STORMS

David, T. W; Ayoade, A. O

dc.contributor.author	David, T. W
dc.contributor.author	Ayoade, A. O
dc.date.accessioned	2022-07-19T10:53:59Z
dc.date.available	2022-07-19T10:53:59Z
dc.date.issued	2008
dc.identifier.citation	David, T. W. & Ayoade, A. O. (2008). RESPONSE OF THE IONOSPHERE TO INTENSE GEOMAGNETIC STORM. International Journal of Natural and Applied Sciences, 4(1): 86-91MS	en_US
dc.identifier.uri	http://localhost:8080/xmlui/handle/123456789/789
dc.description.abstract	Recent 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 simultaneity	en_US
dc.description.sponsorship	T. W. David and A. O. Ayoade	en_US
dc.language.iso	en	en_US
dc.publisher	International Journal of Natural and Applied Sciences	en_US
dc.relation.ispartofseries	4;1
dc.subject	: Geomagnetic storms, solar wind plasma, magnetosphere, ionosphere	en_US
dc.title	RESPONSE OF THE IONOSPHERE TO INTENSE GEOMAGNETIC STORMS	en_US
dc.type	Article	en_US