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Inundation and Damage by Run-up Tsunami of 2011 in the Sendai Plain, Japan

机译:日本仙台平原的洪水海啸淹没和损坏

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After the tsunami of the 2011 off the north-east Japan Earthquake, a survey of the disaster in the residential area of the coastal plain of Miyagi Prefecture was carried out. The damage of structures is explained by photos. It emerges that the tsunami height is more than 8 m on the shore, the inundation depth decreases along the run-up distance as far as 4 km inside from the coast and the state of the houses in the Yuriage town changes at 1.2 km from the coast from destructed into surviving. An experimental record of run-up tsunami suggests that a velocity at the front of tsunami is very strong at a shoreline.
机译:2011年日本东北地震海啸后,进行了宫城县沿海平原住宅区灾难调查。通过照片解释了结构的损害。它出现了海啸高度超过8米的岸边,沿着沿着沿着4公里的淹没深度减少到海岸,阳光镇的房屋的状态距离酒店有1.2公里从破坏的海岸幸存下来。 Run-Up Tsunami的实验记录表明海啸前面的速度在海岸线上非常强烈。

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