日本地球惑星科学連合2014年大会

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セッション記号 M (領域外・複数領域) » M-IS ジョイント

[M-IS26_29AM1] 大気電気学

2014年4月29日(火) 09:00 〜 10:45 422 (4F)

コンビーナ:*芳原 容英(電気通信大学 大学院情報理工学研究科)、牛尾 知雄(大阪大学大学院工学研究科情報通信工学部門)、座長:芳原 容英(電気通信大学 大学院情報理工学研究科)

10:15 〜 10:30

[MIS26-06] 蔵王で観測された北陸冬季雷と関係する下部電離圏におけるLF波の乱調

*森永 洋介1土屋 史紀1小原 隆博1三澤 浩昭1 (1.東北大学 惑星プラズマ大気研究センター)

キーワード:lightning, subionospheric perturbations, electromagnetic pulses, quasi-electrostatic fields

Intense electromagnetic pulses (EMP) radiated from lightning discharge could cause heating and ionization and alter the conductivity in the ionospheric D-region. Quasi-electrostatic fields (QE Fields) which are generated due to the removal of electric charge could also affect it. The purpose of this study is to reveal influence of the lightning on the lower ionosphere and its dependence on properties of lighting discharges. The VLF/LF signature of subionospheric perturbations associated with winter lightning in the Sea of Japan (around Hokuriku) has been observed during December 16-31, 2009. LF (60kHz) radio observation was made at Zao (Miyagi) for Haganeyama JJY transmitter (border between Saga and Fukuoka) whose great circle path (GCP) passes over the coast area of Hokuriku. The amplitude and phase of the JJY signal are recorded every 0.1 seconds. In addition to the subionospheric LF observation, lightning locations are determined by a lightning location network (WWLLN). The number of total lightning event identified in the area of 35-37 degrees N and 134-137 degrees E is 1002. Based on the LF observation, subionospheric perturbations which occur immediately after the causative lightning (early event) were detected. The number of the total detection of the early event in the selected area is 72. Early events identified will be compared with peak current and charge moment of the causative lighting which are derived from LF and ELF waveform observations, respectively, to investigate the relation between early event properties and magnitude of EMP and QE fields.