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dc.contributor.authorO.J. Olwendo
dc.contributor.authorP. Baki
dc.contributor.authorC. Mito
dc.contributor.authorP. Doherty
dc.date.accessioned2012-10-24T09:10:46Z
dc.date.available2012-10-24T09:10:46Z
dc.date.issued2012-08
dc.identifier.citationJournal of Atmospheric and Solar-Terrestrial Physics Volumes 84–85, August 2012, Pages 52–61en_US
dc.identifier.urihttp://hdl.handle.net/123456789/339
dc.descriptionThe original publication is available at http://www.sciencedirect.com/science/article/pii/S1364682612001460en_US
dc.description.abstractThe ionosphere Total Electron Content (TEC), derived by analyzing dual frequency signals from the Global Positioning System (GPS) recorded from two stations in the Kenyan region is studied. We present the mean diurnal, monthly, seasonal, and annual variation in the ionospheric TEC during the lowest solar activity phase for the periods of 2009–2010. Seasonal variations in daytime TEC show a semiannual periodicity, with minimum in June solstice and maxima in March equinox and December solstice. Using mean hourly monthly TEC, we found semiannual variation with two maxima occurring in months of April–March, and September–October. Seasonal variations in the nighttime TEC reveal semiannual periodicity with high background levels observed in the equinoctial months and low background levels in solstice. Results of seasonal variations and month-to-month variations in TEC have been compared with the TEC derived from the IRI-2007 model using the NeQuick option for the topside electron density. The IRI–TEC is too high for all the seasons except for the March equinox where there seems to be good agreement between observation and model. The model is in good agreement with the monthly variation but overestimates for the months of May, June, July, August and September for all the years studied. The minimum monthly mean is lowest in the model for all the months by about 3–5 TECU in comparison to the GPS–TEC. We attribute this to the fact that the model excludes TEC from the plasmasphere while the overestimation of TEC has been associated to overestimation of the equatorial ion fountain effect and also the inability of the model to predict localized (regional) ionospheric effects arising from electromagnetic forcing at the low latitude.en_US
dc.description.sponsorshipPwani Universityen_US
dc.language.isoenen_US
dc.publisherElsevieren_US
dc.subjectGPS–TEC;en_US
dc.subjectLow-latitude;en_US
dc.subjectSeasonal variations;en_US
dc.subjectIRI–TECen_US
dc.titleCharacterization of ionospheric GPS Total Electron Content (GPS–TEC) in low latitude zone over the Kenyan region during a very low solar activity phaseen_US
dc.typeArticleen_US


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