4.7 Article

Geomorphological response of sandy beach to tropical cyclones with different characteristics

Journal

FRONTIERS IN MARINE SCIENCE
Volume 9, Issue -, Pages -

Publisher

FRONTIERS MEDIA SA
DOI: 10.3389/fmars.2022.1010523

Keywords

tropical cyclones; sandy beach; FVCOM; TCs' track; hydrodynamic change

Funding

  1. National Natural Science Foundation of China [42076179, 41476030]
  2. Shandong Key Research and Development Program [2019GHY112057]
  3. Project of Taishan Scholar
  4. research on investigation and prevention of typical sandy coast erosion in Haiyang City [QX1532443]
  5. Laboratory for Marine Geology Open Fund
  6. Flux of suspended particles of Shandong Peninsula [MGQNLM-KF201812]

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This study investigates the response of Haiyang Beach in the northern China Seas to two tropical cyclones, Lekima and Bavi, which passed through different sides of the study area. The study finds that the characteristics of the tropical cyclones have different effects on the beach, with significant changes observed after Lekima but little changes after Bavi. The results suggest that the relative position of the beach and the tracks of the tropical cyclones play a primary role in determining their impact on beaches.
Tropical cyclones (TCs) play important roles in the evolution of beaches. The response of beaches to a single tropical cyclone (TC) has been well reported, however, few studies have compared the responses of the same beach to TCs with different characteristics. Taking Haiyang Beach in the northern China Seas as a case study, the beach profiles before and after two TCs, Lekima and Bavi, which passed through the west and east sides of the study area, were investigated. The beach exhibited erosion at the upper foreshore and minor deposition near the mean high water level (MHW) after Lekima with subaqueous sandbars formed in the nearshore zone, whereas all the beach profiles showed little changes after Bavi. A high-resolution FVCOM model was established and eleven sensitive experiments were conducted to simulate hydrodynamic changes induced by TCs with different tracks, intensity and duration. Then the Xbeach model was used to display the beach evolution due to different TCs conditions. It is found that the significant storm surge and strong seaward bottom current induced by landward wind of the TCs passed through the west side of the study area should responsible for the beach profile changes. Negligible storm surge rise and landward bottom current related to the seaward wind of eastern path TCs can only result in little change of the beach. Swell contributes most to the wave height while has less effect on the beach changes. In this study, we conclude that the effects of TCs on beaches are primarily dependent on relative position of a beach and TCs' tracks.

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