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dc.contributor.authorKelleher, RF
dc.contributor.authorMartin, P
dc.date.accessioned2014-04-29T09:13:45Z
dc.date.available2014-04-29T09:13:45Z
dc.date.issued1975-08
dc.identifier.citationJournal of Atmospheric and Terrestrial Physics Volume 37, Issue 8, August 1975, Pages 1109–1116en_US
dc.identifier.urihttp://www.sciencedirect.com/science/article/pii/0021916975901567
dc.identifier.urihttp://hdl.handle.net/11295/66141
dc.description.abstractFresnel-type fading patterns have been observed on recordings of geostationary and travelling satellites made at three low-latitude stations in East Africa. The occurrence is greatest in the time periods 05–08 and 18–22 local time, at the June solstice. The patterns seem to be produced by patches of increased ionization some 1.5–25 km in extent at heights corresponding to sporadic-E levels and the lower F-region. The sizes show an increase with height. On occasions the patterns exhibit repetition with intervals of 4–30 min. The equations used in determining the height of the patches are reviewed. The results are compared with those from middle latitudes. A possible connection with sporadic-E is discussed.en_US
dc.language.isoenen_US
dc.publisherUniversity of Nairobien_US
dc.titleFresnel-type Fading On Satellite Records At Low Latitudesen_US
dc.typeArticleen_US


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