日本地球惑星科学連合2019年大会

講演情報

[J] 口頭発表

セッション記号 S (固体地球科学) » S-EM 固体地球電磁気学

[S-EM19] 電気伝導度・地殻活動電磁気学

2019年5月27日(月) 09:00 〜 10:30 304 (3F)

コンビーナ:相澤 広記(九州大学大学院理学研究院附属・地震火山観測研究センター)、松野 哲男(神戸大学海洋底探査センター)、座長:松野 哲男相澤 広記

09:45 〜 10:00

[SEM19-04] Referenceデータが与える地磁気変換関数への影響について

*佐藤 真也1後藤 忠徳1 (1.京都大学大学院工学研究科)

キーワード:電流源の空間特性、地磁気変換関数、リモートリファレンス

It is well-known that inter-station transfer functions (TFs), which are derived generally using two sites (as following Schmucker 1984; Neska 2006), are effected by source field. Also, we sometimes use three sites for deriving TFs in order to reduce the noises mixed in geomagnetic data. These 2 or 3 sites-based TFs have been used for evaluating the spatial characteristics of source field. However, the 3 sites-based TFs (i.e., using site 1, site 2 and reference site) do not always reflect the source field’s condition between site 1 and site 2, and can possibly be effected by the source field’ characteristics at reference site. Also, the evaluation of source field’s condition at time-frequency domain (i.e., at the stage of spectra or spectrograms) will be more accurate. Therefore, for the evaluation we used Multi-Channel Nonnegative Matrix Factorization (MC-NMF, suggested by Sato and Goto 2018), which can extract components included in several geomagnetic spectrograms. Moreover, we derived the condition of geomagnetic events’ spatial-characteristics, which triggers the effect of reference data on 3 sites-based TFs. In order to verify that the TFs are effected by the reference site, we derived the temporal changes in 3 sites-based TFs replacing the reference sites. As a result, we founded that the TFs changed not only temporally but dependent on the reference site and the interpretation of source field’s spatial characteristics was different dependent on the reference site. For exposing the cause, we evaluated the spatial-characteristics of geomagnetic events using MC-NMF. The evaluated spatial-characteristics of geomagnetic events were corresponding with the condition triggering the effect of reference data on TFs as mentioned above. We succeeded to expose the cause of TFs’ variation triggered by reference data evaluating the spatial-characteristics of geomagnetic events at time-frequency domain. Using TFs together with MC-NMF, the interpretation of source-field’s spatial characteristics will be with high accuracy.