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Profile response to storm events of sandy beach: observation and modelling
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Junli Guo1, 2, Shenliang Chen3, Qinghua Ye4, Yang Chang5, Lianqiang Shi1, 2, *
Haiyang Xuebao | 2025, 47(2) : 69 - 84
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Haiyang Xuebao | 2025, 47(2): 69-84
Profile response to storm events of sandy beach: observation and modelling
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Junli Guo1, 2, Shenliang Chen3, Qinghua Ye4, Yang Chang5, Lianqiang Shi1, 2, *
Affiliations
  • 1Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou 310012, China
  • 2Key Laboratory of Ocean Space Resource Management Technology, Ministry of Natural Resources, Hangzhou 310012, China
  • 3State Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai 200241, China
  • 4Deltares, Delft 2614HV, the Netherlands
  • 5School of Hydraulic Engineering, Zhejiang University of Water Resources and Electric Power, Hangzhou 310018, China
Published: 2025-02-28 doi: 10.12284/hyxb2025015
Outline
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Beach erosion under the influence of frequent and severe storm events is generally increasing. Understanding the process of beach profile change under the influence of storm events is essential for the protection of sandy coast erosion. To clarify the response characteristics of the embayed beach profile to the storm, this study combined field observation during the typhoon and the XBeach model to reveal the profile morphological changes of the Dongsha beach in Zhujiajian Island, Zhejiang Province, under the influence of typhoon Tapah, and the influence of different factors on the beach storm response was discussed. The main results are as follows. Under the influence of typhoon Tapah, the profile of the Dongsha beach showed a significant pattern of erosion in the upper part of the profile and accretion in the lower part, and there was almost no change in the topography on the seaward side of the 400 m offshore (sand-mud transition). The calculation of different storm scenarios shows that the significant wave height controls the erosion and deposition amplitude of the profile, while the tidal level controls the position of erosion and deposition on the profile. When the storm wave height is large, the difference in profile changes caused by different settings of fine to medium sand grain size range is small. The offshore distance of the stop point of profile change is farther when there is beach nourishment. The results of this study can provide a scientific reference for the protection of storm erosion in the sandy coast.

beach storm response  /  profile change process  /  typhoon Tapah  /  XBeach model
Junli Guo, Shenliang Chen, Qinghua Ye, Yang Chang, Lianqiang Shi. Profile response to storm events of sandy beach: observation and modelling[J]. Haiyang Xuebao, 2025 , 47 (2) : 69 -84 . DOI: 10.12284/hyxb2025015
Year 2025 volume 47 Issue 2
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Article Info
doi: 10.12284/hyxb2025015
  • Receive Date:2024-08-21
  • Online Date:2025-10-27
  • Published:2025-02-28
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History
  • Received:2024-08-21
  • Revised:2024-12-28
Funding
Affiliations
    1Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou 310012, China
    2Key Laboratory of Ocean Space Resource Management Technology, Ministry of Natural Resources, Hangzhou 310012, China
    3State Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai 200241, China
    4Deltares, Delft 2614HV, the Netherlands
    5School of Hydraulic Engineering, Zhejiang University of Water Resources and Electric Power, Hangzhou 310018, China
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表12种不同金属材料的力学参数

Family
属数
Number of
genus
种数
Number of
species
占总种数比例
Percentage of
total species (%)

Genus
种数
Number of
species
占总种数比例
Percentage of total
species (%)
鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78
小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39
多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39
红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87
小菇属 Mycena 11 5.26
光柄菇属 Pluteus 5 2.39
红菇属 Russula 17 8.13
栓菌属 Trametes 5 2.39
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