4.5 Article

Flow separation and roughness lengths over large bedforms in a tidal environment: A numerical investigation

期刊

CONTINENTAL SHELF RESEARCH
卷 91, 期 -, 页码 57-69

出版社

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.csr.2014.09.001

关键词

Tidal dunes; Recirculation zone; Numerical modelling

资金

  1. DFG-Research Center/Cluster of Excellence The Ocean in the Earth System
  2. Danish Council for Independent Research/Natural Sciences [10-081102]
  3. GLOMAR, Bremen International Graduate School for Marine Sciences

向作者/读者索取更多资源

This study characterises the shape of the flow separation zone (FSZ) and wake region over large asymmetric bedforms under tidal flow conditions. High resolution bathymetry, flow velocity and turbulence data were measured along two parallel transects in a tidal channel covered with bedforms. The field data are used to verify the applicability of a numerical model for a systematic study using the Delft3D modelling system and test the model sensitivity to roughness length. Three experiments are then conducted to investigate how the FSZ size and wake extent vary depending on tidally-varying flow conditions, water levels and bathymetry. During the ebb, a large FSZ occurs over the steep lee side of each bedform. During the flood, no flow separation develops over the bedforms having a flat crest; however, a small FSZ is observed over the steepest part of the crest of some bedforms, where the slope is locally up to 15 degrees. Over a given bedform morphology and constant water levels, no FSZ occurs for velocity magnitudes smaller than 0.1 m s(-1); as the flow accelerates, the FSZ reaches a stable size for velocity magnitudes greater than 0.4 m s(-1). The shape of the FSZ is not influenced by changes in water levels. On the other hand, variations in bed morphology, as recorded from the high-resolution bathymetry collected during the tidal cycle, influence the size and position of the FSZ: a FSZ develops only when the maximum lee side slope over a horizontal distance of 5 m is greater than 10. The height and length of the wake region are related to the length of the FSZ. The total roughness along the transect lines is an order of magnitude larger during the ebb than during the flood due to flow direction in relation to bedform asymmetry: during the ebb, roughness is created by the large bedforms because a FSZ and wake develops over the steep lee side. The results add to the understanding of hydrodynamics of natural bedforms in a tidal environment and may be used to better parameterise small-scale processes in largescale studies. (C) 2014 Elsevier Ltd. All rights reserved.

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