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岬湾沙滩地貌对台风响应的数值模拟研究

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台风作用下的岬湾沙滩地貌变化较为复杂,厘清岬湾沙滩地貌对台风响应过程与机理具有重要理论意义与现实意义.基于XBeach软件构建台风作用下的岬湾沙滩地貌变化数值模型,在较好验证的基础上模拟东沙沙滩地貌对"利奇马"台风作用的响应过程,进而探析泥沙输移和地貌变化的机理.研究表明:台风登陆前后潮位和台风浪强度对岬湾沙滩的地貌变化起主导作用,在这2个因素的共同作用下,沙滩上部侵蚀明显,泥沙整体向离岸方向运动,并在沙滩下部淤积.产生的裂流在台风期间台风浪与风暴潮条件下,会对沙滩造成较大程度的侵蚀,落潮期间的落潮流在沿岸泥沙的输移中也起着重要作用.岬角掩蔽区域波浪动能减弱是台风作用下该区域出现泥沙淤积的主要原因.
Numerical Study of Geomorphologic Evolution Induced by Typhoon in Embayed Beach
The geomorphologic evolution induced by typhoon in embayed beach is complicated;it is of great theoretical and practical significance to clarify the response process and mechanism.In this paper,we constructed a numerical model of geomorphologic evolution under the typhoon in embayed beach based on XBeach software,and simulated the response process of Dongsha beach geomorphology to Super Typhoon Lekima.Then we analyzed the mechanism of sediment transport and geomorphologic evolution.The study shows that the tidal level and the strength of the typhoon waves play a dominant role in the geomorphologic evolution in embayed beach,and that under the combined effect of these two factors,the upper part of the beach(foreshore)erodes significantly,and the overall movement of the sediment moves offshore,and siltation occurs in the lower part of the beach(backshore).The rip currents cause a greater degree of beach erosion under typhoon wave and storm surge conditions,and the currents during low tide also play an important role in sediment transport along the shoreline.The weakening of wave kinetic energy in the sheltered area of the headland is the main reason for the occurrence of sedimentation.

embayed beachnumerical studygeomorphologic evolutiontyphoon effectXBeach

陈大喜、黄君宝、刘旭、张炜、姚文伟、何睿杭

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三门县水利局,浙江 三门 317100

浙江省水利河口研究院(浙江省海洋规划设计研究院),浙江 杭州 310017

浙江省河口海岸重点实验室,浙江 杭州 310017

平阳县水利局,浙江 平阳 325400

河海大学,江苏 南京 210098

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岬湾沙滩 数值模拟 地貌变化 台风影响 XBeach

浙江省水利厅科技计划项目

RB2215

2024

浙江水利科技
浙江省水利河口研究院 浙江省水利学会

浙江水利科技

影响因子:0.294
ISSN:1008-701X
年,卷(期):2024.52(3)