Journal article

Modeling of suspended sediment concentrations under combined wave-current flow over rippled bed

J Lu, XH Wang, AV Babanin, S Aijaz, Y Sun, Y Teng, KT Jung, F Qiao

Estuarine Coastal and Shelf Science | ACADEMIC PRESS LTD- ELSEVIER SCIENCE LTD | Published : 2017

Abstract

Ripples appear and disappear dynamically on coastal bed. The bottom stress can significantly be enhanced when ripples appear, and then the sediment transport will be influenced by the ripple-enhanced stress. However, ripples’ impact on suspended sediments is seldom discussed. In this study, a bedform (ripples) module based on combined wave and current flow is coupled with a bottom boundary layer (BBL) model. This BBL model outputs our improved bottom shear stress (BSS) to both the sediment model (UNSW-sed) and the hydrodynamic model (POM). Model results in Jervis Bay of Australia show that the simulated suspended sediment concentration (SSC) of an abrupt rising is significantly improved by c..

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University of Melbourne Researchers

Grants

Awarded by National Natural Science Foundation of China


Funding Acknowledgements

This is a Sino-Australian Research Centre for Coastal Management Publication No. 40. This work is supported by the Project supported by the National Natural Science Foundation of China (Grant No. 1606405), by Fundamental Research Funds For National Public Research Institutes of China (2014T01, 2015P03), by the National key R&D Program of China (2017YFC1404202), and by the China-Korea Cooperation Project for the nuclear safety funded by CKJORC. This work is also supported by the NSFC-Shandong Joint Fund for Marine Science Research Centers (U1406404) and by the National Program on Global Change and Air-Sea Interaction (GASI-IPOVAI-05). The corresponding author F Qiao was supported by International cooperation project on the China-Australia Research Centre for Maritime Engineering of Ministry of Science and Technology (2016YFE0101400) and Qingdao National Laboratory for Marine Science and Technology (2015ASTP, 2016ASKJ16 and 2015ASKJ01). We also acknowledge ADV, ADCP and sediment data from Geoscience Australia.