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首页> 外文期刊>Geomorphology >Tsunami-induced morphological change - A model-based impact assessment of the 1755 tsunami in NE Atlantic from the Morocco coast
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Tsunami-induced morphological change - A model-based impact assessment of the 1755 tsunami in NE Atlantic from the Morocco coast

机译:海啸引起的形态变化-基于模型的摩洛哥海岸东北大西洋1755年海啸影响评估

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摘要

Tsunamis can be responsible for coastal geomorphic crises. Extensively inundated coasts can suffer widespread and dramatic changes in their morphology due to sediment erosion, transport, and deposition processes. In this paper, we investigate the tsunami-induced morphological changes on coasts prone to inundation and how sediment transport is controlled by both tsunami and sediment characteristics. We focus on a tsunami-prone coast in the NE Atlantic, Tangier-Morocco, that experienced the 1755 Lisbon tsunami. We use a coupled hydrodynamic and morphodynamic numerical model, together with high-resolution digital elevation and sedimentary models, to simulate the impact of tsunamis on the morphology and sediment distribution of Tangier Bay. Due to the uncertainty on the source and effects of the 1755 event, we consider two 1755-like tsunamigenic scenarios that have the potential to cause different levels of inundation. Results show that the coastal zone of Tangier can undergo substantial changes in morphology and sediment distribution following the tsunami impact. For the selected scenarios, the volume of sediments mobilized, at both the offshore and onshore zones of the Tangier site, ranges from 30,000 to 200,000 m(3). Moreover, the presence of mobile sediments and conditions favoring tsunami shoaling lead to an increase in wave impact on the coastal configuration. Conversely, the presence of the breakwaters helps to protect the Tangier coast by limiting the extent of the affected area. The results of this study suggest that the assessment of tsunami-induced coastal impact should include the effect on morphology. (C) 2018 Elsevier B.V. All rights reserved.
机译:海啸可能是造成海岸地貌危机的原因。由于沉积物的侵蚀,运输和沉积过程,泛滥的沿海地区的形态可能会发生广泛而剧烈的变化。在本文中,我们研究了海啸引起的容易被淹没的海岸的形态变化,以及海啸和沉积物特征如何控制沉积物的运输。我们将重点放在丹吉尔摩洛哥东北部大西洋海啸多发海岸,该海岸经历了1755年里斯本海啸。我们使用耦合的水动力和形态动力数值模型,以及高分辨率的数字高程和沉积模型,来模拟海啸对丹吉尔湾的形态和沉积物分布的影响。由于1755年事件的来源和影响的不确定性,我们考虑了两种类似1755年海啸的情景,它们有可能导致不同程度的淹没。结果表明,由于海啸的影响,丹吉尔沿海地区的形态和沉积物分布可能发生重大变化。对于选定的方案,在丹吉尔站点的近海和陆上区域动员的沉积物量为30,000至200,000 m(3)。此外,流动性沉积物的存在和有利于海啸浅滩的条件导致波浪对沿海构造的影响增加。相反,防波堤的存在有助于通过限制受灾地区的范围来保护丹吉尔海岸。这项研究的结果表明,海啸引起的沿海影响的评估应包括对形态的影响。 (C)2018 Elsevier B.V.保留所有权利。

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