Modeling of inundation dynamics on Banda Aceh, Indonesia during the great Sumatra tsunamis December 26, 2004
Modeling of inundation dynamics on Banda Aceh, Indonesia during the great Sumatra tsunamis December 26, 2004
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2004 年 12 月 26 日苏门答腊海啸期间印度尼西亚班达亚齐洪水动态建模
DOI：
10.1007/s11069-010-9710-7
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发表时间：
2011
期刊：
影响因子：
3.7
通讯作者：
T. Healy
中科院分区：
文献类型：
--
作者：
G. Prasetya;J. Borrero;W. Lange;K. Black;T. Healy
2004年12月26日，印度尼西亚班达亚齐的海啸淹没了内陆5公里，摧毁了沿海沿着的大部分房屋、建筑物和基础设施，造成167，000多人死亡。据幸存者报告，来自西北海岸和西海岸的陆上水流在距离Ulee Lheue（西北海岸）约3.7公里和距离Lhok Nga（西海岸）约6.8公里的Lampisang村相撞。基于非线性浅水波方程的淹没模拟再现了淹没模式，并展示了漫流的碰撞。该模型表明，班达亚齐西北海岸的波浪特征与影响西海岸的波浪特征不同。这些地区，经历了较高的淹没水平，并不总是经历最大的陆上流速，和损坏的地区大多符合流速分布，而不是助跑和淹没深度。
The tsunami inundation flows on Banda Aceh, Indonesia reached 5 km inland during the December 26, 2004, event and devastated most of the houses, buildings, and infrastructure along the coast and killed more than 167,000 people. The overland flows from the northwest coast and the west coast collided at Lampisang village approximately 3.7 km from Ulee Lheue (northwest coast) and 6.8 km from Lhok Nga (west coast) as reported by survivors. Inundation modeling based on the nonlinear shallow-water wave equations reproduces the inundation pattern and demonstrates a colliding of the overland flows. The model suggests that wave characteristics on the northwest coast of Banda Aceh were different from those on the waves that impacted upon the west coast. The areas, which experienced higher inundation levels, did not always experience greatest overland flow speeds, and the damage areas mostly coincide with the flow speed distribution rather than the runup and inundation depth.
影响因子：
3
作者：
Fujii, Yushiro;Satake, Kenji
通讯作者：
Satake, Kenji
根据海啸波形估算2004年苏门答腊-安达曼大地震的破裂过程
DOI：
--
发表时间：
2006
期刊：
Earth Planet Space 58
影响因子：
--
作者：
Tanioka;Y.;Nishimura;Y.
通讯作者：
Y.