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Geospace perturbations induced by the Earth: The state of the art and future trends
Institution:1. Istituto Nazionale di Geofisica e Vulcanologia, V. Vigna Murata 605, 00143 Roma, Italy;2. ASI, Rome, Italy;3. Università di Trento, Italy;4. INFN, sez. Perugia and ASI Science Data Centre, Frascati, Italy;5. UniNettuno, Roma, Italy;6. LPC2E/CNRS, France;7. IAASARS, National Observatory of Athens, Athens, Greece;8. IAPS-INAF, Roma, Italy;9. Università G. D’Annunzio, Chieti, Italy;10. School of Electronic Information, Wuhan University, China;11. Space Science Institute, School of Astronautics, Beihang University, China;1. Charles University, Faculty of Mathematics and Physics, V Holesovickach 2, 180 00 Prague, Czech Republic;2. University of Texas at Arlington, Texas, TX 76019, USA;3. Institute of Atmospheric Physics, Czech Academy of Sciences, Bocni II 1401, 141 31 Praha 4, Czech Republic;4. National Central University, Institute of Space Science, 300 Jhongda Road, Jhongli, Taoyuan 32001, Taiwan;1. Università di Bologna “Alma Mater Studiorum”, Viale Berti Pichat 6/2, 40126 Bologna, Italy;2. Istituto Nazionale di Geofisica e Vulcanologia, Via di Vigna Murata 605, 00143 Roma, Italy;3. Universidade do Vale do Paraiba (UNIVAP), IP&D, São José dos Campos, SP, Brazil;4. CIASUR, Facultad Regional Tucumán, Universidad Tecnológica Nacional, Argentina;5. Laboratorio de Ionósfera, Universidad Nacional de Tucumán, Argentina;6. CONICET, Buenos Aires, Argentina;7. Laboratorio de Telecomunicaciones, Universidad Nacional de Tucumán, Argentina
Abstract:A systematic multi-parameter and multi-platform approach to study the slow process of earthquake preparation is fundamental to gain some insights on this complex phenomenon. In particular, an important contribution is the integrated analysis between ground geophysical data and satellite data. In this paper we review some of the more recent results and suggest the next directions of this kind of research. Our intention is not to detect a particular precursor but to understand the physics underlying the various observations and to establish a reliable physical model of the preparation phase before an impending earthquake. In this way, future investigation will search for suitable fore-patterns, which the physical model of multi-layers coupling predicts and characterizes by quasi-synchronism in time and geo-consistency in space. We also present alternative explanations for some anomalies which are not actually related to earthquakes, rather to other natural or anthropic processes.
Keywords:Earthquake physics  Lithosphere–atmosphere–ionosphere coupling  Seismic precursors  Integrated earthquake study
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