Evolution of tidal system and material transport off the Huanghe River Delta induced by human activities and natural evolution

Miao Hongbing; Qiao Lulu; Zhong Yi; Li Guangxue

doi:10.12284/hyxb2022071

Volume 44 Issue 9

Aug. 2022

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Miao Hongbing，Qiao Lulu，Zhong Yi, et al. Evolution of tidal system and material transport off the Huanghe River Delta induced by human activities and natural evolution[J]. Haiyang Xuebao，2022, 44(9)：73–86 doi: 10.12284/hyxb2022071

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Evolution of tidal system and material transport off the Huanghe River Delta induced by human activities and natural evolution

doi: 10.12284/hyxb2022071

Miao Hongbing^1
,,
Qiao Lulu^{1, 2
,
,},
Zhong Yi^{1, 3},
Li Guangxue^{1, 2}

1.
College of Marine Geosciences, Ocean University of China, Qingdao 266100, China
2.
The Key Lab of Sea Floor Resource and Exploration Technique, Ministry of Education, Qingdao 266100, China
3.
Yellow Sea Fisheries Research Institute, Chinese Academy of Fishery Sciences, Qingdao 266001, China

Received Date: 2021-08-22
Rev Recd Date: 2022-01-10

Available Online: 2022-04-12

Publish Date: 2022-08-29

Abstract

Abstract

In recent years, the topography of Huanghe River Delta exhibits significant changes due to natural and man-made reasons, such as delta acceleration and dyke construction. At the same time, these factors also lead to important variations in the tidal wave system and material transport path in the adjacent sea area. In this study, we establish a three-dimensional high-resolution tide, current and Lagrangian particle tracking numerical model of the Huanghe River Delta and its adjacent sea area based on FVCOM. Our modeling results agree well with the tidal harmonic constant of the tide gauge stations in Bohai Sea region and the observation data of tide level stations and current stations in the Huanghe River Delta. Thus, this model can reflect the characteristics of tide and tidal current in the Huanghe River Delta and its adjacent sea area. Furthermore, the location of the 2019 amphidromic point of M₂ is also obtained from this model. By designing five numerical experiments of natural coastline evolution, dyke construction and corresponding water depth changes in the Huanghe River Delta in 1980 and 2019, the following conclusions are drawn. Firstly, from 1980 to 2019, the amphidromic point of M₂ moves southeast, with the major factor of water depth. Secondly, changes of coastal line caused by the extension of the Huanghe River Estuary and the construction of dykes have minor effects to the location of amphidromic point of M₂. Nevertheless, these changes can form the residual current gyres on both sides of the convex bank. As a result, the material from the Huanghe River stays longer in Laizhou Bay and delays its transportation and diffusion to Bohai Sea.
- Huanghe River Delta,
- amphidromic point evolution,
- FVCOM,
- material transport

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References(29)

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