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Atmosphere, ocean and lithosphere interaction as a possible drive of earthquake triggering 被引量:1
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作者 Victor Volkov Jan Mrlina +3 位作者 Mstislav Dubrov Vladimir Smirnov sergey golovachev Vaclav Polak 《Geodesy and Geodynamics》 2020年第6期442-454,共13页
The comparison of tiltmeter and strainmeter data in the periods of the strongest earthquakes with tropical cyclone activities in the World Ocean during Januarye April 2014 is made.Main features of the observed co-seis... The comparison of tiltmeter and strainmeter data in the periods of the strongest earthquakes with tropical cyclone activities in the World Ocean during Januarye April 2014 is made.Main features of the observed co-seismic tilt and strain processes are consistent with the results obtained for the strongest events during 1997-2004.The time-frequency data analysis and the comparison of the analysis results with the anomalous geomagnetic and ionospheric activity come to an agreement with the observed phenomena.The obtained results have allowed the triggering mechanism of seismicity to be proposed.The process begins as spatial and temporal swings of the regions of tropical cyclone origins and the basins of their activity.The powerful cyclone development accompanies a wide range of earthquake precursory phenomena,including abnormal behavior of ultra-wideband(0.002 m Hz-3 Hz)Earth’s oscillations,which can be recorded at far distances up to 1000-10,000 km.The daily dissipation energy of the most powerful tropical cyclone(hurricane,typhoon)is estimated to have same order of magnitude as the energy released by an event of Mw 7-9,as well,atmospheric depressions are big enough to trigger a forthcoming strong earthquake.The triggering mechanism could be caused by quasi-static and timedependent surface loading that produces vertical tension and shear deformations.This loading affects the seafloor and coastline where they fall close to the adjacent tectonic plate boundaries. 展开更多
关键词 Tilt and strain Tropical cyclone Earthquake HURRICANE
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