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Lithosphere-atmosphere-ionosphere coupling as governing mechanism for preseismic short-term events in atmosphere and ionosphere

机译:岩石圈 - 气氛 - 电离层耦合作为大气和电离层中苛性的短期事件的控制机制

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We present a general concept of mechanisms of preseismic phenomena in the atmosphere and ionosphere. After short review of observational results we conclude: 1. Upward migration of fluid substrate matter (bubble) can lead to ousting of the hot water/gas near the ground surface and cause an earthquake (EQ) itself in the strength-weakened area; 2. Thus, time and place of the bubble appearance could be random values, but EQ, geochemistry anomaly and foreshocks (seismic, SA and ULF electromagnetic ones) are casually connected; 3. Atmospheric perturbation of temperature and density could follow preseismic hot water/gas release resulting in generation of atmospheric gravity waves (AGW) with periods in a range of 6–60min; 4. Seismo-induced AGW could lead to modification of the ionospheric turbulence and to the change of over-horizon radio-wave propagation in the atmosphere, perturbation of LF waves in the lower ionosphere and ULF emission depression at the ground.
机译:我们在大气和电离层中提出了沉重的衰老现象机制的一般概念。在短暂审查观察结果后,我们得出结论:1。液体基材物质(泡沫)向上迁移可以导致地面靠近地面附近的热水/气体,并在强度弱化区域中引起地震(EQ)本身;因此,泡沫外观的时间和地点可能是随机值,但随机连接,等式,地球化学异常和牧师(地震,SA和ULF电磁器); 3.温度和密度的大气扰动可遵循早期的热水/气体释放,导致大气重力波(AGW)的时间为6-60分钟; Seismo诱导的Agw可能导致改变电离层湍流以及在大气中改变大气中的过度范围的无线波繁殖,LF波在地下较低的电离层和ULF发射凹陷中的LF波的扰动。

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