Numerical estimation of source current intensity causing ULF emissions associated with earthquakes by using WLP-FDTD method
Author:
Affiliation:
1. The University of Electro-Communications
2. Chiba University
3. Hayakawa Institute of Seismo Electromagnetics Co. Ltd.
Publisher
Institute of Electrical Engineers of Japan (IEE Japan)
Subject
General Medicine
Link
https://www.jstage.jst.go.jp/article/jae/41/2/41_52/_pdf
Reference21 articles.
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2. 2) Bleier T., C. Dunson, M. Maniscalco, N. Bryant, R. Bambery, and F. Freund (2009), Investigation of ULF magnetic pulsations, air conduc¬tiv¬ity changes, and infra red signatures associ¬ated with the 30 October Alum Rock M5.4 earthquake, Nat. Haz. Earth Sys. Sci., 9, pp. 585-603
3. 3) Chung Y. S., T. K. Sarkar, B. H. Jung, and M. Salazar-Palma (2003), An unconditionally stable scheme for the finite-difference time-domain method, IEEE Trans. Microwave Tech. Theory, 51, pp. 697-704
4. 4) Di Giacomo D., E. R. Engdahl, and D. A. Storchak (2018). The ISC-GEM Earthquake Catalogue (1904-2014): status after the Exten¬sion Project, Earth Syst. Sci. Data, 10, pp. 1877-1899, doi: 10.5194/essd-10-1877-2018
5. 5) Fraser-Smith A. C., A. Bernardi, P. R. McGill, M. E. Ladd, R. A. Helliwell, and O. G. Villard, Jr. (1990), Low-frequency magnetic field measurements near the epicenter of the Ms 7.1 Loma Prieta earthquake, Geophys. Res. Lett., 17(9), pp. 1465-1468
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1. A Numerical Consideration on the Correlation Between Magnitude of Earthquakes and Current Intensity Causing ULF Electromagnetic Wave Emission;Radio Science;2024-07
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