The reflection of obliquely incident tsunamis
The reflection of obliquely incident tsunamis
复制标题
倾斜入射海啸的反射
DOI：
10.1017/s0022112083001834
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发表时间：
1983
影响因子：
3.7
通讯作者：
C. F. Noiseux
中科院分区：
文献类型：
--
作者：
G. Carrier;C. F. Noiseux
当海啸入射到平面陆架上时，反射波的波形和振幅与入射波的波形和振幅有很大的不同，当陆架具有真实的大陆架的极不规则特征时，两者之间的反差更大。在这里，我们量化这些声明，我们也给一个帐户的方式，其中运行取决于的结晶度和其他参数的入射波的特征。
When a tsunami is incident on a plane shelf, the waveform and amplitude of the reflected wave differ significantly from those of the incident wave, and, when the shelf has the extremely irregular character of real continental shelves, the contrast between the two amplitudes is even greater. Here we quantify these statements and we also give an account of the manner in which the run-up depends on the obliquity and on other parameters characterizing the incident wave.