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Tsunami Risk Map-a Case Sstudy of Gongliao District

机译:海啸风险图-以贡lia区为例

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摘要

A great tsunami had stroke the northern coast of Taiwan in 1867. Thestudy area is focused on Gongliao District, New Taipei City. Theassumed earthquake scenario originated from Yap Trench is used forCornell University tsunami model (COMCOT model) which simulatesthe wave height and wave speed of the tsunami triggered by theearthquake. The wave heights of the northern coast of Taiwan are thenused as boundary conditions for overland flow simulation. Risk due totsunami is defined as hazard multiplying by vulnerability. Themaximum water depth, the maximum water speed due to tsunami andrising rate of water surface level are used for production of tsunamihazard map. As for vulnerability, population and habitat environmentare taken into account. After evaluating hazard and vulnerability, thehigh tsunami risk area can be delineated, and can take suitablemeasures to reduce loss of life and properties.
机译:1867年,一场大海啸席卷了台湾北部海岸。 研究区域以新北市公ong区为重点。这 假设源自Yap Trench的地震情景用于 康奈尔大学海啸模型(COMCOT模型),用于模拟 海啸引发的海啸的波高和波速。 地震。那么台湾北部沿海的波高为 用作陆流模拟的边界条件。由于的风险 海啸的定义是危害乘以脆弱性。这 最大水深,海啸和海啸造成的最大水速 水面水位上升率被用于生产海啸 危害图。关于脆弱性,人口和栖息地环境 被考虑在内。在评估危害和脆弱性之后, 可以划定高海啸风险区,并采取适当的措施 减少生命和财产损失的措施。

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