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dc.contributor.authorDavid, T. W.-
dc.contributor.authorAdedokun, V. O.-
dc.date.accessioned2022-07-19T10:19:18Z-
dc.date.available2022-07-19T10:19:18Z-
dc.date.issued2009-
dc.identifier.citationDavid, T. W. & Adedokun, V. O. (2009). EFFECT OF LOCAL TIME ON THE F2 -REGION RESPONSE TO THE GEOMAGNETIC STORM OF JANUARY 28, 1985. International Journal of Natural and Applied Sciences, 5(3): 244-250en_US
dc.identifier.urihttp://localhost:8080/xmlui/handle/123456789/783-
dc.description.abstractThe F2-region response to the storm of January 28, 1985, was investigated in this research using some ionospheric stations from East Asian and Euro-African sectors. The sectors were chosen because of their huge time difference, which enabled the proper identification of whether or not plasma is redistributed owing to sunrise effect when a storm occurs. The storm occurred around 14:00 universal time (UT), which corresponded with local time (LT) of Euro-African sector of between 1-4 p.m. and 10-11 p.m. of East Asian sector. From the result obtained, it was concluded that sunrise effect could redistribute the plasma when a geomagnetic storm occurs due to the fact that the three low latitude stations in Euro-African behaved in an undefined manner, while the response of the East Asian stations agreed with existing theoriesen_US
dc.description.sponsorshipT. W. David and V. O. Adedokunen_US
dc.language.isoenen_US
dc.publisherInternational Journal of Natural and Applied Sciencesen_US
dc.relation.ispartofseries5;3-
dc.subjectF2-region, geomagnetic storm, universal time, local time, ionospheric stationsen_US
dc.titleEFFECT OF LOCAL TIME ON THE F2 -REGION RESPONSE TO THE GEOMAGNETIC STORM OF JANUARY 28, 1985en_US
dc.typeArticleen_US
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