Physics
Scientist
Physics Department, University of Western Ontario, London, Ontario, Canada
University of Western Ontario, Ont., N6A 5B9, London, Canada
University of Western Ontario, London, Canada
Department of Physics, University of Wales, Aberystwyth, SY23 3BZCeredigionUK, GBHigh Altitude Observatory, NCAR, Boulder, COUSA, USInstitute of Space and Atmospheric Studies, University of Saskatchewan, SaskatoonCanada, CAInstitute for Meteorology, University of Leipzig, LeipzigGermany, DEInstitute for Geophysics and Geology, University of Leipzig, Collm ObservatoryGermany, DEUniversity of New Hampshire, DurhamUSA, USUniversity of Western Ontario, LondonCanada, CABritish Antarctic Survey, NERC, CambridgeUK, GBUniversity of Adelaide, AdelaideAustralia, AUAlbinos-Institute of Atmospheric Physics, KühlungsbornGermany, DECommunications Research Laboratory, Koganei, TokyoJapan, JPUniversity of Canterbury, ChristchurchNew Zealand, NZRadio Science Centre for Space and Atmosphere, KyotoJapan, JPInstitute for Experimental Meteorology, ObninskRussia, RUKazan State University, KazanRussia, RURhodes University, GrahamstownSouth Africa, ZAKharkov State Technical University of Radioelectronics, KharkovUkraine, GBColorado Research Associates, Boulder, COUSA, US
Institute of Space and Atmospheric Studies, University of Saskatchewan, S7N 5E2SaskatoonCanada, CADefence Research Establishment Ottawa, OttawaCanada, CADepartment of Physics and Astronomy, University of Western Ontario, LondonCanada, CA
Department of Physics and Astronomy, University of Western Ontario, London, Canada
Department Electrical Engineering, Univ. Western Ontario, London, ont n6a3k7, Canada
Department of Electrical Engineering, University of Western Ontario, London, Canada
Department Electrical Engineering, Univ. Western Ontario, London, on n6a5b9, Canada
Department of Physics and Astronomy, University of, Western Ontario, Canada
Univ. Western Ontario, Dep. Electrical Engineering Univ. Western Ontario, London, ON n6a 5b9, Canada
D
An explanation for the seasonal dependence of midlatitude sporadic E layers
Conjugate Sporadic-E measurements
Effects of a “day-time” substorm on the ionosphere and radio propagation
Equatorial plasma fountain and its effects over three locations: Evidence for an additional layer, the <formula>F3 layer
Global-scale tidal structure in the mesosphere and lower thermosphere during the PSMOS campaign of June-August 1999 and comparisons with the global-scale wave model
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