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Modeling of Tsunami Generation and Propagation by a Spreading Curvilinear Seismic Faulting in Linearized Shallow-Water Wave Theory

机译:线性化浅水波理论中传播曲线地震断裂的海啸发生与传播的建模

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The processes of tsunami evolution during its generation in search for possible amplification mechanisms resulting from unilateral spreading of the sea floor uplift is investigated. We study the nature of the tsunami build up and propagation during and after realistic curvilinear source models represented by a slowly uplift faulting and a spreading slip-fault model. The models are used to study the tsunami amplitude amplification as a function of the spreading velocity and rise time. Tsunami waveforms within the frame of the linearized shallow water theory for constant water depth are analyzed analytically by transform methods (Laplace in time and Fourier in space) for the movable source models. We analyzed the normalized peak amplitude as a function of the propagated uplift length, width and the average depth of the ocean along the propagation path.
机译:研究了海啸演变过程中的海啸演变过程,以寻找由海床隆起的单方面扩散引起的可能的放大机制。我们研究了以缓慢隆升断层和扩展滑动断层模型为代表的实际曲线源模型期间和之后海啸累积和传播的性质。这些模型用于研究海啸振幅放大率与传播速度和上升时间的关系。通过转换方法(时间上的拉普拉斯和空间上的傅立叶),针对可移动源模型,分析了线性化浅水理论框架内恒定水深的海啸波形。我们分析了归一化的峰值振幅,它是沿着传播路径传播的隆起长度,宽度和海洋平均深度的函数。

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