Physics
Scientist
Communications Research Laboratory, Research Alliance Office, Strategic Planning Division, 4-2-1 Nukui-Kita, Koganei, Tokyo 184-8795, Japan
Communications Research Laboratory, Tokyo, Japan
National Institute of Information and Communications Technology, Tokyo, Japan
Communications Research Laboratory Koganei-shi, Tokyo 184, Japan
Communication Research Laboratory Tokyo, Japan
Communications Research Laboratory, Koganei, Tokyo, Japan
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
Communications Research Laboratory, Independent Administrative Institution, 4-2-1 Nukui-Kitamachi, Koganei-Shi, 184-8795TokyoJapan, JP
Communications Research Laboratory, 4-2-1 Nukui Kita, Koganei, Tokyo 184-8795, Japan
Communications Research Laboratory, Upper Atmospheric Section, Space Science Division, 4-2-1 Nukui-kitamachi Koganei-shi, Tokyo, Japan
Collaborative Research Management Department, National Institute of Information and Communica
24- and 12-h oscillations during a time of strong eastward wind in the upper mesosphere at 31° and 45° N
A comparative study of global ionospheric responses to intense magnetic storm conditions
A large-scale traveling ionospheric disturbance during the magnetic storm of 15 September 1999
Amplitude variations in GPS signals as a possible indicator of ionospheric structures
Analytic method for observation of the gravity waves using radio occultation data
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