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首页> 外文期刊>Journal of Coastal Research: An International Forum for the Littoral Sciences >Barrier island geomorphology, hydrodynamic modelling, and historical shoreline changes: An example from South Uist and Benbecula, Scottish outer hebrides
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Barrier island geomorphology, hydrodynamic modelling, and historical shoreline changes: An example from South Uist and Benbecula, Scottish outer hebrides

机译:屏障岛的地貌,水动力模型和历史海岸线变化:以南乌伊斯特和本贝库拉为例,苏格兰外赫布里底群岛

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摘要

Dawson, A.G.; Gómez, C.; Ritchie, W.; Batstone, C.; Lawless, M.; Rowan, J.S.; Dawson, S.; Mcilveny, J.; Bates, R., and Muir, D., 2012. Barrier island geomorphology, hydrodynamic modelling, and historical shoreline changes: an example from South Uist and Benbecula, Scottish Outer Hebrides. A partly quantitative reconstruction is provided of the evolution of Gualan Island, a barrier island located between South Uist and Benbecula in the Scottish Outer Hebrides, using historical maps, aerial photographs, and Lidar (light detection and ranging) data. Geomorphological changes over the last approximately 200 years are described together with quantitative changes in the dimension of the barrier island, including rates of shoreline retreat. A series of digital terrain models (DTMs) provided the boundary conditions for a two-dimensional (2D) ocean circulation tide-surge model simulating water level and wave conditions associated with a highly destructive storm that took place during January 2005. During this storm event, the central part of the barrier island was overtopped by waves. Validating the hydrodynamic model against eye-witness and field evidence obtained after the 2005 storm allowed simulation of a range of potential future breaching scenarios. Thus with the same storm conditions a large barrier breach 500 m wide would result in wave heights rising by 0.8-0.9 m on hitherto sheltered shorelines.
机译:A.G.道森; C.Gómez;里奇(W.) Batstone,C .;无法无天,M。罗恩,J.S .;道森,S。 Mcilveny,J .; Bates,R.和Muir,D.,2012年。障壁岛地貌,流体动力学建模和历史海岸线变化:苏格兰南外赫布里底群岛南尤斯特和本贝库拉的例子。使用历史地图,航拍照片和激光雷达(测光和测距)数据,对位于苏格兰外赫布里底群岛南乌伊斯特和本贝库拉之间的隔离岛瓜兰岛的演化提供了部分定量重建。描述了过去约200年的地貌变化以及屏障岛的大小(包括海岸线撤退率)的定量变化。一系列数字地形模型(DTM)为二维(2D)海洋环流潮涌模型提供了边界条件,该模型模拟了与高度破坏性风暴相关的水位和波浪条件,发生于2005年1月。 ,屏障岛的中心部分被海浪覆盖。根据目击者和现场证据对水动力模型进行验证,可以模拟2005年以后可能发生的一系列破坏事件。因此,在相同的暴风雨条件下,一个大的500 m宽的障碍物突破口将导致迄今为止庇护的海岸线上的波高上升0.8-0.9 m。

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