A large‐scale traveling ionospheric disturbance during the magnetic storm of 15 September 1999
A large‐scale traveling ionospheric disturbance during the magnetic storm of 15 September 1999
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DOI:
10.1029/2001ja000245
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发表时间:
2002-06
影响因子:
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通讯作者:
K. Shiokawa;Y. Otsuka;T. Ogawa;N. Balan;K. Igarashi;A. Ridley;D. Knipp;A. Saito;K. Yumoto
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文献类型:
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作者:
K. Shiokawa;Y. Otsuka;T. Ogawa;N. Balan;K. Igarashi;A. Ridley;D. Knipp;A. Saito;K. Yumoto
enhancement of GPS total electron content (� 1.0 � 10 16 m � 2 ). Multipoint and imaging observations of these parameters show that the LSTID moved equatorward over Japan with a velocity of � 400–450 m/s. From a comparison with the Sheffield University Plasmasphere-Ionosphere Model (SUPIM) we conclude that an enhancement (250–300 m/s) of poleward neutral wind (that is propagating equatorward) caused these observational features of the LSTID at midlatitudes. To investigate generation of the LSTID by auroral energy input, we have used auroral images obtained by the Polar UVI instrument, magnetic field variations obtained at multipoint ground stations, and the empirical Joule heating rate calculated by the assimilative mapping of ionospheric electrodynamics (AMIE) technique. Intense auroral energy input was observed at 0800–1100 UT (4–6 hours before the LSTID), probably causing equatorward neutral wind at lower latitudes. It is likely that the poleward wind pulse that caused the observed LSTID was generated associated with the cessation of this equatorward wind. The effect of Lorentz force is also discussed. INDEX TERMS: 0310 Atmospheric Composition and Structure: Airglow and aurora; 2427 Ionosphere: Ionosphere/atmosphere interactions (0335); 2435 Ionosphere: Ionospheric disturbances; 2437 Ionosphere: Ionospheric dynamics; 2788 Magnetospheric Physics: Storms and substorms; KEYWORDS: large-scale traveling ionospheric disturbance, thermosphere–ionosphere coupling, magnetic storm, airglow imaging, GPS network, ionosonde