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On the Resonant Behavior of a Weakly Compressible Water Layer During Tsunamigenic Earthquakes

机译:关于海啸地震期间弱可压缩水层的共振行为

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摘要

Tsunamigenic earthquakes trigger pressure waves in the ocean, given the weak compressibility of the sea water. For particular conditions, a resonant behavior of the water layer can occur, which influences the energy transfer from the sea-bed motion to the ocean. In this paper, the resonance conditions are explained and analyzed, focusing on the hydro-acoustic waves in the proximity of the earthquake area. A preliminary estimation of the generation parameters (sea-bed rising time, velocity) is given, by means of parametric numerical simulations for simplified conditions. The results confirm the importance of measuring, modeling, and interpreting such waves for tsunami early detection and warning.
机译:考虑到海水的弱压缩性,海啸地震会在海洋中触发压力波。在特定条件下,水层可能发生共振行为,从而影响从海床运动到海洋的能量传递。本文以地震区附近的水声波为重点,对共振条件进行了解释和分析。通过简化条件下的参数数值模拟,对发电参数(海床上升时间、速度)进行了初步估算。这些结果证实了测量、建模和解释此类波对海啸早期探测和预警的重要性。

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