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dc.contributor.authorKelleher, R. F.
dc.contributor.authorRöttger, J.
dc.date.accessioned2013-06-28T15:17:27Z
dc.date.available2013-06-28T15:17:27Z
dc.date.issued1973
dc.identifier.citationJournal of Atmospheric and Terrestrial Physicsen
dc.identifier.urihttp://dx.doi.org/10.1016/0021-9169(73)90017-2
dc.identifier.urihttp://erepository.uonbi.ac.ke:8080/xmlui/handle/123456789/41995
dc.description.abstractDuring February and April 1972, 3 weeks of observations of irregularity patches were made by two methods: 1. (a) Non-great-circle propagation on the transequatorial path Lindau-Tsumeb; 2. (b) Radar backscatter at Nairobi. A comparison of the results shows high correlation in the occurrence of events observed, the correlation reaching a maximum at 2130 local Nairobi time. A detailed example of the movement of patches is given for one particular day. The significance of the results is discussed.en
dc.language.isoenen
dc.relation.ispartofseriesVolume 35, Issue 6, June 1973, Pages 1207–1211;
dc.titleEquatorial spread-F irregularities observed at Nairobi and on the transequatorial path Lindau-Tsumeben
dc.typeArticleen
local.publisherDepartment of Physics, University of Nairobien


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