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Erosion and Accretion on a Mudflat: The Importance of Very Shallow-Water Effects
Shi, B.; Cooper, J.R.; Pratolongo; Gao, S.; Bouma, T.J.; Li, G.; Li, C.; Yang, S.L.; Wang, Y. (2017). Erosion and Accretion on a Mudflat: The Importance of Very Shallow-Water Effects. Journal of Geophysical Research-Oceans 122(12): 9476–9499. https://dx.doi.org/10.1002/2016jc012316
In: Journal of Geophysical Research-Oceans. AMER GEOPHYSICAL UNION: Washington. ISSN 2169-9275, meer
Peer reviewed article  

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  • NIOZ: NIOZ files 310326
  • NIOZ: NIOZ Open Repository 310327 [ beschikbaar vanaf 01/07/2018 ]

Author keywords
    Bed-level change; Bed shear stress; Very shallow-water stage; Open intertidal mudflat; China coast

Auteurs  Top 
  • Shi, B.
  • Cooper, J.R.
  • Pratolongo
  • Gao, S.
  • Bouma, T.J., meer
  • Li, G.
  • Li, C.
  • Yang, S.L.
  • Wang, Y.

Abstract
    Understanding erosion and accretion dynamics during an entire tidal cycle is important for assessing their impacts on the habitats of biological communities and the long-term morphological evolution of intertidal mudflats. However, previous studies often omitted erosion and accretion during very shallow-water stages (VSWS, water depths < 0.20 m). It is during these VSWS that bottom friction becomes relatively strong and thus erosion and accretion dynamics are likely to differ from those during deeper flows. In this study, we examine the contribution of very shallow-water effects to erosion and accretion of the entire tidal cycle, based on measured and modeled time-series of bed-level changes. Our field experiments revealed that the VSWS accounted for only 11% of the duration of the entire tidal cycle, but erosion and accretion during these stages accounted for 35% of the bed-level changes of the entire tidal cycle. Predicted cumulative bed-level changes agree much better with measured results when the entire tidal cycle is modeled than when only the conditions at water depths of >0.2 m (i.e., probe submerged) are considered. These findings suggest that the magnitude of bed-level changes during VSWS should not be neglected when modeling morphodynamic processes. Our results are useful in understanding the mechanisms of micro-topography formation and destruction that often occur at VSWS, and also improve our understanding and modeling ability of coastal morphological changes.

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