Hydroacoustic measurements highlight channel impact on macrotidal mudflat morphodynamics
ID:260 View Protection:ATTENDEE Updated Time:2024-12-31 20:58:16 Hits:795 Poster Presentation

Start Time:2025-01-16 20:35(Asia/Shanghai)

Duration:15min

Session:S17 Session 17-Advances in Coastal Hydrodynamics and Sediment Dynamics for a Sustainable Ocean » S17-PAdvances in Coastal Hydrodynamics and Sediment Dynamics for a Sustainable Ocean

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Abstract
Unvegetated tidal mudflats are typically dissected by networks of channels that arguably exert a prominent role in the ecomorphodynamic evolution of these environments. However, the intricate processes of tidal flows propagating through tidal channels and across mudflat platforms remain inadequately understood, particularly concerning the localized hydrodynamics occurring at the interface between channels and mudflats. In this study, we report the results of in-situ hydroacoustic measurements carried out in the macrotidal Yangkou tidal flat (Jiangsu coast, China), where we synchronously assessed the three-dimensional flow fields and suspended sediment concentrations at three distinct sites—namely, the channel thalweg, channel bank, and distant mudflat platform—over the course of 8 semidiurnal tidal cycles. Whereas mudflat areas typically exhibit an overall flood dominance, tidal channels feature ebb-dominated flows and higher concentrations of suspended sediments. In contrast to vegetated tidal settings, where in-channel flow velocities are systematically higher than across the frictionally dominated intertidal plains, hydrodynamics of bare mudflat systems is controlled by flow inertia and sheet-flow conditions whenever water levels exceed the channel bankfull threshold. At bankfull, pronounced changes in tidal flow orientation are observed, which critically enhance both cross-sectional velocities within the channel and bottom shear stress near channel banks. Our results support earlier suggestions that the hydrodynamics of bare mudflat systems are strongly influenced by the interactions between in-channel and overbank flows. Therefore, we propose that future modeling works related to accurately reproducing morphodynamic processes occurring in unvegetated coastal environments should take into account the localized three-dimensional flow interactions near the channel-flat interface.
Keywords
intertidal mudflats, tidal channels, tidal asymmetry, sediment transport, hydroacoustic
Speaker
Chao Gao
Postdoctor Nanjing University

Submission Author
Chao Gao Nanjing University
Alvise Finotello University of Padova
Ya Ping Wang Nanjing University
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Important Date
  • Conference Date

    Jan 13

    2025

    to

    Jan 17

    2025

  • Sep 27 2024

    Draft paper submission deadline

  • Feb 17 2025

    Registration deadline

Sponsored By
State Key Laboratory of Marine Environmental Science, Xiamen University
Organized By
State Key Laboratory of Marine Environmental Science, Xiamen University
Department of Earth Sciences, National Natural Science Foundation of China
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