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The synergy of earthquake precursors
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作者 Sergey Pulinets 《Earthquake Science》 CSCD 2011年第6期535-548,共14页
The system of geophysical shells (lithosphere, atmosphere, ionosphere) is considered as an open complex nonlinear system with dissipation where earthquake preparation could be regarded as a self-organizing process l... The system of geophysical shells (lithosphere, atmosphere, ionosphere) is considered as an open complex nonlinear system with dissipation where earthquake preparation could be regarded as a self-organizing process leading to the critical state of the system. The processes in atmosphere and ionosphere are considered from the point of view of non-equilibrium thermodynamics. The intensive ionization of boundary layer of atmosphere (probably provided by radon in occasion of earthquake preparation) gives start to the synergetic sequence of coupling processes where the ionosphere and even magnetosphere are the last links in the chain of interactions. Every anomaly observed in different geophysical fields (surface temperature, latent heat flux, electromagnetic emissions, variations in ionosphere, particle precipitation, etc.) is not considered as an individual process but the part of the self-organizing process, the final goal of which is the reaching of the point of the maximum entropy. Radon anomaly before the Kobe earthquake is considered as a perfect example to satisfy the formal seismological determination of the earthquake precursor. What is genetically connected with radon through the ionization process can also be regarded as a precursor. The problem of co-seismic variations of the discussed parameters of atmosphere and ionosphere is considered as well. 展开更多
关键词 SYNERGY earthquake precursor complex system RADON ENTROPY critical state
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The Role of the Dipole Interaction of Molecules with Charged Particles in the Polar Stratosphere
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作者 Yury Belikov Sergey Nikolayshvili 《Journal of Earth Science and Engineering》 2016年第3期115-149,共35页
关键词 平流层气溶胶 偶极相互作用 带电粒子 单极性 光化学过程 氯氧化物 宇宙射线 平衡浓度
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Atmosphere-ionosphere response to the M9 Tohoku earthquake revealed by multiinstrument space-borne and ground observations:Preliminary results 被引量:9
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作者 Dimitar Ouzounov Sergey Pulinets +5 位作者 Alexey Romanov Alexander Romanov Konstantin Tsybulya Dmitri Davidenko Menas Kafatos Patrick Taylor 《Earthquake Science》 CSCD 2011年第6期557-564,共8页
We retrospectively analyzed the temporal and spatial variations of four different physical parameters characterizing the state of the atmosphere and ionosphere several days before the M9 Tohoku, Japan earthquake of Ma... We retrospectively analyzed the temporal and spatial variations of four different physical parameters characterizing the state of the atmosphere and ionosphere several days before the M9 Tohoku, Japan earthquake of March 11, 2011. The data include outgoing long wave radiation (OLR), GPS/TEC, lower Earth orbit ionospheric tomography and critical frequency foF2. Our first results show that on March 7th a rapid increase of emitted infrared radiation was observed from the satellite data and an anomaly developed near the epicenter. The GPS/TEC data indicate an increase and variation in electron density reaching a maximum value on March 8. Starting from this day in the lower ionosphere also there was confirmed an abnormal TEC variation over the epicenter. From March 3 to 11 a large increase in electron concentration was recorded at all four Japanese ground-based ionosondes, which returned to normal after the main earthquake. The joint preliminary analysis of atmospheric and ionospheric parameters during the M9 Tohoku, Japan earthquake has revealed the presence of related variations of these parameters implying their connection with the earthquake process. This study may lead to a better understanding of the response of the atmosphere/ionosphere to the great Tohoku earthquake. 展开更多
关键词 Tohoku earthquake thermal anomaly GPS/TEC earthquake precursor early warning
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Improvements in Inversion of Magnetic Resonance Exploration-Water Content, Decay Time, and Resistivity 被引量:1
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作者 Ugur Yaramanci Mike Müller-Petke 《Journal of China University of Geosciences》 SCIE CSCD 2009年第3期592-605,共14页
In this review article, we present recent developments and improvements in magnetic resonance sounding (MRS), a newly established geophysical exploration method that provides unique information about hydrogeophysica... In this review article, we present recent developments and improvements in magnetic resonance sounding (MRS), a newly established geophysical exploration method that provides unique information about hydrogeophysical properties due to its direct sensitivity to hydrogen protons and proton dynamics. Starting with the most sophisticated and complete MRS formulation, we give a detailed view on how to solve the equation, i.e., inverting exactly for all model parameters: water content, decay time, and resistivity. Giving a short review of general inversion schemes used in geophysics, the special properties of MRS inversion are evaluated and the development of MRS inversion over recent years is shown. We present the extension of MRS to magnetic resonance tomography (MRT), i.e., the extension to two-dimensional investigations and appropriate inversions. Finally, we address restrictions, limitations, and inconsistencies as well as future developments. 展开更多
关键词 magnetic resonance sounding (MRS) magnetic resonance tomography (MRT) INVERSION MODELING water content decay time resistivity.
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