Response process of the Haiyang Beach evolution to Typhoon Lekima in Shandong Province

Gao Wei; Li Ping; Gao Shan; Tian Ziwen; Li Bing; Liu Jie; Xu Yuanqin

doi:10.3969/j.issn.0253-4193.2020.11.009

Volume 42 Issue 11

Dec. 2020

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Gao Wei，Li Ping，Gao Shan, et al. Response process of the Haiyang Beach evolution to Typhoon Lekima in Shandong Province[J]. Haiyang Xuebao，2020, 42(11)：88–99 doi: 10.3969/j.issn.0253-4193.2020.11.009

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Response process of the Haiyang Beach evolution to Typhoon Lekima in Shandong Province

doi: 10.3969/j.issn.0253-4193.2020.11.009

Gao Wei^{1, 2
,},
Li Ping^{1, 2
,
,},
Gao Shan^{1, 2},
Tian Ziwen³,
Li Bing⁴,
Liu Jie^{1, 2},
Xu Yuanqin^{1, 2}

1.
Key Laboratory of Marine Geology and Metallogeny, First Institute of Oceanography, Ministry of Natural Resources, Qingdao 266061, China
2.
Laboratory for Marine Geology, Pilot National Laboratory for Marine Science and Technology (Qingdao), Qingdao 266237, China
3.
Coastal Science and Marine Policy Center, First Institute of Oceanography, Ministry of Natural Resources, Qingdao 266061, China
4.
Island Research Center, Ministry of Natural Resources, Pingtan 350400, China

Received Date: 2020-02-27
Rev Recd Date: 2020-05-07

Available Online: 2020-12-03

Publish Date: 2020-11-25

Abstract

Abstract

By using the beach monitoring technologies such as Unmanned Aerial Vehicle (UAV) and elevation monitoring equipment, the monitoring data of Haiyang beach before and after Typhoon Lekima (No.1909) were obtained, the morphology changes, erosion and accretion variation of beach profiles during Typhoon Lekima landing were analyzed, and the response of beach evolution to the typhoon was discussed. The result shows that beach morphology evolution after the typhoon is mainly including the expansion of the aeolian dune area, erosion of the beach surface in the high-middle tidal zone, micro-topography disappearance and so on. The typhoon mainly affected the beach by erosion, resulting in an erosion volume about 2.43×10⁴ m³, which mainly occurred on the high tide zone. The aeolian dunes were weakly silted, but some of them were eroded seriously. The backshore was weakly silted because of sand deposition from strong wind and alluvial flow. In the middle and low tide zones, beach morphology changes were mainly controlled by the beach surfaces lope, which was manifested as erosion with high slope, weak deposition with low slope, and several small sandbanks formed after the typhoon. On the whole, the typhoon impacts on the beach evolution mainly lead to the sediment budget deficit, and further exacerbated the erosion of Haiyang beach.
- Typhoon Lekima,
- Haiyang City,
- beach evolution,
- beach erosion

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References(40)

References

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