Modelling tsunami induced coarse clast transport , combination of physical experiments, advanced numerical modelling and field observations

虽然沿海地区对人口和工业具有很大的吸引力，但它们也极易受到极端波浪事件（海啸、风暴潮）的影响。考虑到预期的人口和工业持续增长，迫切需要高精度地评估频率-震级关系和损害潜力。根据这些评估，可以制定灾害管理计划和减轻灾害战略。尽管高强度海啸可能造成灾难性的影响，但其重复发生的时间间隔在数百年至数千年之间。因此，在历史记录较短的特定海岸，可能无法对这种最坏情况进行观测或测量。在这种情况下，沉积在岸上的海洋沉积物提供了极端洪水事件的证据。通过将特定的沉积物特性与颗粒运动所需的波能相联系，可以推导出引起沉积物输运（海啸或风暴潮/波浪形成）的水动力过程的独特特性。由于陆上块体和巨砾作为细沉积物更能抵抗侵蚀和人类影响，因此更适合进行此类调查。然而，在大多数情况下，区分风暴和海啸是一项坚韧的任务。数值模型可以支持这样的解释，但仍然受到一些简化，如忽略沉积负荷，多个漂砾或复杂的漂砾形状之间的相互作用。此外，这些因素在最先进的物理实验室实验中也被忽视。同样，只有实验利用理想形状的身体模型均匀形状的测深和沿海地形是know.The拟议的项目旨在弥合四个实质性的差距，在国家的最先进的。首先，行为（i）复杂和理想化的模型巨石和（ii）它们之间的相互作用在海啸助跑将进行分析和比较实验室实验。巨石运输模式，路径和距离的影响，由于（iii）不均匀的水深设置和（iv）沉积负荷的调查随后。下一步包括通过使用物理实验的结果来开发、校准和验证数值两相模型。根据摄影技术记录和数字实施的地形和块沉积数据，该模型应能够在项目结束时以前所未有的准确度模拟海啸引发的运输事件。对于项目后的未来，该模型的应用是打算在博内尔岛（荷属安的列斯群岛），那里的沿海巨石沉积学已经非常详细的记录。

While coastal areas are highly attractive for population and industry, they are also highly exposed to extreme-wave events (tsunamis, storm surges). Considering the expected continuing population and industrial growth, there is an urgent need to assess frequency-magnitude relationships and damage potentials with high accuracy. Based on such assessments, it is possible to develop hazard management plans and hazard-mitigation strategies. Even though high-magnitude tsunamis may cause disastrous impacts, their recurrence intervals are in the range of hundreds to thousand years. Thus, at particular coasts with short historical records, no observations or even measurements of such worst-case scenarios might be available. In this case marine sediments deposited onshore provide, evidence for an extreme-flooding event. By associating specific sediment characteristics with the necessary wave-energy for particle movements, distinct characteristics of the hydrodynamic process inducing the sediment transport (tsunami or storm surge/wave setup-up) can be derived. Since subaerial blocks and boulders are more resistant towards erosion and human impact as fine sediments, they are more suitable for such investigations. However, distinguishing between storm and tsunamis is in most cases a tough task. Numerical models can support such interpretations, but still suffer from several simplifications as negligence of sedimentary load, interactions between multiple boulders or complex boulder shapes. Furthermore, these factors are also neglected in state-of-the-art physical laboratory experiments. Likewise, only experiments utilizing idealised shaped body-models on uniform shaped bathymetries and coastal topographies are known.The proposed project aims at bridging four substantial gaps in the state-of-the-art. Firstly, the behaviour of (i) complex and idealised model boulders and (ii) interactions between them during the tsunami runup will be analysed and compared by laboratory experiments. Investigations of the influences on boulder transport mode, path, and distance due to (iii) non-uniform bathymetric settings and (iv) sedimentary load follow afterwards. The next step comprises the development, calibration, and validation of a numerical two-phase model by using results of the physical experiments. Based on photo-technically recorded and numerically implemented data for topography and block deposits, the model shall be able to simulate tsunami-induced transport events with an unprecedented accuracy by project close-out. For the post-project future, the model application is intended for the island of Bonaire (Netherlands Antilles), where the coastal boulder sedimentology is already documented in high detail.