On-Shelf Tsunami Generation and Coastal Propagation
On-Shelf Tsunami Generation and Coastal Propagation
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陆架海啸的产生和沿海传播
DOI：
10.1007/978-94-015-8565-1_1
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发表时间：
1995
期刊：
影响因子：
--
通讯作者：
G. Carrier
中科院分区：
文献类型：
--
作者：
G. Carrier
当沿海地区的地震事件在该地区的倾斜陆架上引发高能海啸时，一部分能量向海传播，一部分能量在震源区旁边的海岸段上表现为上升，然后向海反射，另一部分能量以捕获的“边缘波”形式沿沿着传播，并具有色散衰减。我们在这里量化的宽边助跑和侵蚀，伴随着沿岸传播。
When a seismic event in a coastal region initiates an energetic Tsunami on the sloping shelf of that region, some of the energy propagates seaward, some of it is manifested in the run-up on the coastal segment alongside the source region and then reflected seaward and some of it, in the form of trapped “edge-waves”, propagates along the shelf with a dispersive attenuation. We quantify here the broadside run-up and the encroachment that accompanies the along-shore propagation.