自然筑堤海滩对台风Lekima遭遇不同潮汐类型的形态动力学响应建模

IF 1.6 Q4 ENVIRONMENTAL SCIENCES Anthropocene Coasts Pub Date : 2022-08-24 DOI:10.1007/s44218-022-00004-4
Xu Liu, Cuiping Kuang, Shichang Huang, Weiliang Dong
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引用次数: 4

摘要

XBeach等基于过程的沿海地区模型的最新发展为使用2DH网格预测沿海对风暴水动力等主要强迫机制的响应提供了新的机会。然而,由于缺乏实测数据,模型的应用场景很少。因此,还需要更多的测量和研究。本文选取小潮期袭击浙江的台风“勒基玛”,在假设遇到不同潮型的情况下,模拟了皇城滩的形态动力学响应。具有八个横向海岸剖面的横向海岸测量(命名为S1 ~ 从北到南S8)。然后利用Delft3D流/波建立了二维风暴潮-波浪耦合模型。该模型利用测量的水位和波浪数据进行了很好的校准,并为改进的模型提供了不同台风和潮汐类型耦合情况下的流体动力学边界条件。利用XBeach建立了精细化模型,并对皇城滩的形态响应进行了模拟验证。根据数值结果,分析了八个剖面的床面变化,说明了不同潮汐条件下的冲淤特征。大潮条件下的净沙量变化小于中潮和小潮条件下的变化。对碰撞、淹没和退潮不同阶段波浪诱导流分布的进一步研究表明,大潮条件下更强的水流会增加S3和S6剖面的输沙率并减少沉积量 ~ S8,整个海滩参与运输的沉积物总量增加,导致S1、S2、S4和S5剖面的净侵蚀量减少。
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Modelling morphodynamic responses of a natural embayed beach to Typhoon Lekima encountering different tide types

Recent developments in process-based coastal area models such as XBeach provide new opportunities to predict coastal responses to primary forcing mechanisms such as storm hydrodynamic by using 2DH grids. However, due to the lack of measured data, there are few application scenarios of the models. Therefore, more measurement and research are needed. In this paper, the Typhoon Lekima that hitting Zhejiang Province during neap tide period was selected to simulate morphodynamic responses of the Huangcheng Beach by assuming encountering with different tide types. Cross shore measurements with eight cross-shore profiles (named S1 ~ S8 from north to south) of the Huangcheng Beach pre- and post- the Typhoon Lekima respectively were presented. Then a 2DH storm surge and wave coupled model was established with Delft3D Flow/Wave. The model was well calibrated with measured water levels and wave data and provided hydrodynamic boundary conditions of different typhoon and tide types coupling situations for a refined model. The refined model was built using XBeach and simulated the morphological responses of the Huangcheng beach with well verifications. On basis of the numerical results, bed level changes at the eight profiles were analyzed, and the character of erosion and deposition under different tide conditions were illustrated. The net sand volume changes were got smaller under the spring tide condition rather than middle tide and neap tide conditions. Further study of the distribution of wave induced current at different stages of collision, inundation and ebb shown that the stronger current under spring tide condition would increase the sediment transport rate and reduce the deposition volume at profiles S3 and S6 ~ S8, and the total amount of sediment involved in transportation had increased for the whole beach, leading to the reduction of net erosion volume at profiles S1, S2, S4 and S5.

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