Modeling tidal sand wave formation in a numerical shallow water model: the role of turbulence formulation

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13 Citations (Scopus)

Abstract

Tidal sand waves are prominent dynamic bottom features in shallow sandy seas. Up to now, the processes controlling the formation of these bedforms have only been studied in stability sand wave models, in which geometry, boundary conditions and turbulence models are schematized. In this paper we present simulations of sand wave formation and migration with a numerical shallow water model (Delft3D), in which we restrict us to bedload transport and analyse the initial formation stage only. First, it is shown that the reproduction of the basic sand wave formation mechanisms in a numerical shallow water model requires careful treatment of model geometry, initial profile, vertical resolution and lateral boundary conditions. Second, an intercomparison between the Delft3D model and a nonlinear stability sand wave model is performed. Next, we compare the results for two of the built-in turbulence models: constant vertical eddy viscosity model (commonly used in stability sand wave models) and a more advanced spatially and temporally variable vertical eddy viscosity model (k–ε turbulence model). Finally, the model results are compared with field data on sand wave length. The k–ε turbulence model shows good agreement with the field data, whereas the constant vertical eddy viscosity model overestimates the wave length of the sand waves considerably
Original languageEnglish
Pages (from-to)17-27
JournalContinental shelf research
Volume60
DOIs
Publication statusPublished - 2013

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tidal modeling
sand wave
shallow water
turbulence
sand
water
eddy
viscosity
wavelengths
boundary condition
wavelength
geometry

Keywords

  • METIS-289150
  • IR-86056

Cite this

@article{6a3a365221754fa489bbb24feeae608d,
title = "Modeling tidal sand wave formation in a numerical shallow water model: the role of turbulence formulation",
abstract = "Tidal sand waves are prominent dynamic bottom features in shallow sandy seas. Up to now, the processes controlling the formation of these bedforms have only been studied in stability sand wave models, in which geometry, boundary conditions and turbulence models are schematized. In this paper we present simulations of sand wave formation and migration with a numerical shallow water model (Delft3D), in which we restrict us to bedload transport and analyse the initial formation stage only. First, it is shown that the reproduction of the basic sand wave formation mechanisms in a numerical shallow water model requires careful treatment of model geometry, initial profile, vertical resolution and lateral boundary conditions. Second, an intercomparison between the Delft3D model and a nonlinear stability sand wave model is performed. Next, we compare the results for two of the built-in turbulence models: constant vertical eddy viscosity model (commonly used in stability sand wave models) and a more advanced spatially and temporally variable vertical eddy viscosity model (k–ε turbulence model). Finally, the model results are compared with field data on sand wave length. The k–ε turbulence model shows good agreement with the field data, whereas the constant vertical eddy viscosity model overestimates the wave length of the sand waves considerably",
keywords = "METIS-289150, IR-86056",
author = "Borsje, {Bastiaan Wijnand} and Roos, {Pieter C.} and Wouter Kranenburg and Hulscher, {Suzanne J.M.H.}",
year = "2013",
doi = "10.1016/j.csr.2013.04.023",
language = "English",
volume = "60",
pages = "17--27",
journal = "Continental shelf research",
issn = "0278-4343",
publisher = "Elsevier",

}

Modeling tidal sand wave formation in a numerical shallow water model: the role of turbulence formulation. / Borsje, Bastiaan Wijnand; Roos, Pieter C.; Kranenburg, Wouter; Hulscher, Suzanne J.M.H.

In: Continental shelf research, Vol. 60, 2013, p. 17-27.

Research output: Contribution to journalArticleAcademicpeer-review

TY - JOUR

T1 - Modeling tidal sand wave formation in a numerical shallow water model: the role of turbulence formulation

AU - Borsje, Bastiaan Wijnand

AU - Roos, Pieter C.

AU - Kranenburg, Wouter

AU - Hulscher, Suzanne J.M.H.

PY - 2013

Y1 - 2013

N2 - Tidal sand waves are prominent dynamic bottom features in shallow sandy seas. Up to now, the processes controlling the formation of these bedforms have only been studied in stability sand wave models, in which geometry, boundary conditions and turbulence models are schematized. In this paper we present simulations of sand wave formation and migration with a numerical shallow water model (Delft3D), in which we restrict us to bedload transport and analyse the initial formation stage only. First, it is shown that the reproduction of the basic sand wave formation mechanisms in a numerical shallow water model requires careful treatment of model geometry, initial profile, vertical resolution and lateral boundary conditions. Second, an intercomparison between the Delft3D model and a nonlinear stability sand wave model is performed. Next, we compare the results for two of the built-in turbulence models: constant vertical eddy viscosity model (commonly used in stability sand wave models) and a more advanced spatially and temporally variable vertical eddy viscosity model (k–ε turbulence model). Finally, the model results are compared with field data on sand wave length. The k–ε turbulence model shows good agreement with the field data, whereas the constant vertical eddy viscosity model overestimates the wave length of the sand waves considerably

AB - Tidal sand waves are prominent dynamic bottom features in shallow sandy seas. Up to now, the processes controlling the formation of these bedforms have only been studied in stability sand wave models, in which geometry, boundary conditions and turbulence models are schematized. In this paper we present simulations of sand wave formation and migration with a numerical shallow water model (Delft3D), in which we restrict us to bedload transport and analyse the initial formation stage only. First, it is shown that the reproduction of the basic sand wave formation mechanisms in a numerical shallow water model requires careful treatment of model geometry, initial profile, vertical resolution and lateral boundary conditions. Second, an intercomparison between the Delft3D model and a nonlinear stability sand wave model is performed. Next, we compare the results for two of the built-in turbulence models: constant vertical eddy viscosity model (commonly used in stability sand wave models) and a more advanced spatially and temporally variable vertical eddy viscosity model (k–ε turbulence model). Finally, the model results are compared with field data on sand wave length. The k–ε turbulence model shows good agreement with the field data, whereas the constant vertical eddy viscosity model overestimates the wave length of the sand waves considerably

KW - METIS-289150

KW - IR-86056

U2 - 10.1016/j.csr.2013.04.023

DO - 10.1016/j.csr.2013.04.023

M3 - Article

VL - 60

SP - 17

EP - 27

JO - Continental shelf research

JF - Continental shelf research

SN - 0278-4343

ER -