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2D numerical modelling of bed profile changes due to tsunami effects on near shore coasts: Kadikoy case study

机译:Kadikoy案例研究由于海啸影响而在近岸海岸造成的河床剖面变化的二维数值模拟

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This study was aimed at the investigation of tsunami effects on the seabed profile as these may be important for coastal structures, like sea outfalls or breakwaters. Tsunamis are well known with huge wave heights and destructive effects on the coastal region. A 2D numerical model was set using the software, COSMOS to calculate the cross-shore sediment transport and to evaluate profile changes in the coastal seabed. The study area is Kadikoy region, a densely populated industrial coastal area in South East Istanbul. The model was run for different kinds of tsunami waves. Not only the bed profile changes, but also the wave heights, breaker depths, peak wave bottom orbital velocities, wave set-up and cross-shore sediment transport rates were determined. The results indicated that, at a water depth around 40-50 m, some tsunamis were found to have a wave height of order of 15 m, which became about 5 m at a depth of 10 m. The wave set up near the coast was about 1.5-2 m. The results also implied that tsunami waves, with their destructive nature, could lead to dramatic vertical changes of the seabed.
机译:这项研究的目的是调查海啸对海床剖面的影响,因为这些影响对于沿海结构(如排海口或防波堤)可能很重要。海啸以其巨大的波高和对沿海地区的破坏性作用而闻名。使用COSMOS软件设置了二维数值模型,以计算跨海岸沉积物的迁移并评估沿海海床的剖面变化。研究区域是Kadikoy地区,伊斯坦布尔东南部人口稠密的工业沿海地区。该模型针对不同类型的海啸运行。不仅确定了河床剖面的变化,还确定了波高,破碎机深度,波峰底轨道速度,波的建立和跨岸沉积物的输送速度。结果表明,在40-50 m左右的水深处,发现一些海啸的波高约为15 m,在10 m的深度处变为约5 m。在海岸附近建立的波浪约为1.5-2 m。结果还暗示,海啸波具有破坏性,可能导致海床的垂直变化剧烈。

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