Impact of wave–current coupling on the bottom boundary layer in Bohai Bay

Impact of wave–current coupling on the bottom boundary layer in Bohai Bay

Sediment resuspension primarily occurs within the bottom boundary layer (BBL) of water bodies, particularly in silty coastal environments, and helps form the fluid mud layer (FML). In this study, we report data on the water level, waves, currents, and suspended sediment concentration (SSC) collected...

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Bibliographic Details
Main Authors: Siyu Liu, Guangxue Li, Xue Liu, Lulu Qiao, Nan Wang, Shidong Liu, Xiangdong Wang, Di Yu, Lei Zhang
Format: Article
Language:English
Published: Frontiers Media S.A. 2025-01-01
Series:Frontiers in Marine Science
Subjects:
fluid mud layer
bottom boundary layer
shear stress
sediment resuspension
wave-current coupling
Online Access:https://www.frontiersin.org/articles/10.3389/fmars.2024.1521925/full
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