EFFECT OF LOCAL TIME ON THE F2 -REGION RESPONSE TO THE GEOMAGNETIC STORM OF JANUARY 28, 1985

David, T. W.; Adedokun, V. O.

dc.contributor.author	David, T. W.
dc.contributor.author	Adedokun, V. O.
dc.date.accessioned	2022-07-19T10:19:18Z
dc.date.available	2022-07-19T10:19:18Z
dc.date.issued	2009
dc.identifier.citation	David, 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): 244-250	en_US
dc.identifier.uri	http://localhost:8080/xmlui/handle/123456789/783
dc.description.abstract	The 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 theories	en_US
dc.description.sponsorship	T. W. David and V. O. Adedokun	en_US
dc.language.iso	en	en_US
dc.publisher	International Journal of Natural and Applied Sciences	en_US
dc.relation.ispartofseries	5;3
dc.subject	F2-region, geomagnetic storm, universal time, local time, ionospheric stations	en_US
dc.title	EFFECT OF LOCAL TIME ON THE F2 -REGION RESPONSE TO THE GEOMAGNETIC STORM OF JANUARY 28, 1985	en_US
dc.type	Article	en_US