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Characteristics of Sea Ice floes Run-up caused by Tsunami Considering Ice Jams and Ice Pile-ups around Structures

机译:海啸引起的海浮冰上升特征,考虑结构周围的冰堵和积冰现象

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We performed model experiments on the inundation flow of tsunamiswith ice floes. After the collision force imparted by the ice floes acts onstructures, the tsunami flow is dammed by the formation of ice jamsbetween the structures, and a large static force also acts on thestructures because of the water level rise in front of the structures andbecause of hydrostatic pressure between the structures due to the icejam,and this steady state remains for some time. We developed asimple theoretical model for estimating the water depth and the tsunamiforce, and we verified the validity of the model.
机译:我们对海啸的淹没流进行了模型实验 与浮冰。在浮冰施加的碰撞力作用后 建筑物,海啸的流动被形成的冰封堵住了 在结构之间,并且很大的静力也作用在结构上 由于建筑物前面的水位上升,建筑物和 由于冰冻造成的结构之间的静水压力, 这种稳定状态会保留一段时间。我们开发了 估算水深和海啸的简单理论模型 力,我们验证了模型的有效性。

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