Vertical two-dimensional non-hydrostatic pressure model with single layer
- 130 Downloads
Abstract
The vertical two-dimensional non-hydrostatic pressure models with multiple layers can make prediction more accurate than those obtained by the hydrostatic pres-sure assumption. However, they are time-consuming and unstable, which makes them unsuitable for wider application. In this study, an efficient model with a single layer is developed. Decomposing the pressure into the hydrostatic and dynamic components and integrating the x-momentum equation from the bottom to the free surface can yield a horizontal momentum equation, in which the terms relevant to the dynamic pressure are discretized semi-implicitly. The convective terms in the vertical momentum equation are ignored, and the rest of the equation is approximated with the Keller-box scheme. The velocities expressed as the unknown dynamic pressure are substituted into the continuity equation, resulting in a tri-diagonal linear system solved by the Thomas algorithm. The validation of solitary and sinusoidal waves indicates that the present model can provide comparable results to the models with multiple layers but at much lower computation cost.
Key words
vertical two-dimensional model non-hydrostatic pressure single layer Thomas algorithm waveChinese Library Classification
O3522010 Mathematics Subject Classification
76M20Preview
Unable to display preview. Download preview PDF.
References
- [1]Kang, L. and Guo, X. M. Hydrodynamic effects of reconnecting lake group with Yangtze River in China. Water Sci. Eng., 4(4), 405–420 (2011)MathSciNetGoogle Scholar
- [2]Kang, L. and Guo, X. M. Study on water diversion schemes of large urban lake group (in Chinese). Journal of Hydroelectric Engineering, 31(3), 65–69 (2012)MathSciNetGoogle Scholar
- [3]Ai, C. F. and Jin, S. Three-dimensional non-hydrostatic model for free surface flows with unstructured grid. J. Hydrodyn., 20(1), 108–116 (2008)CrossRefGoogle Scholar
- [4]Mahadevan, A., Oliger, J., and Street, R. A non-hydrostatic mesoscale ocean model, part.: well posedness and scaling. Journal of Physical Oceanography, 26(9), 1868–1880 (1996)CrossRefGoogle Scholar
- [5]Zhou, J. G. and Stansby, P. K. An arbitrary Lagrangian-Eulerian σ (ALES) model with nonhydrostatic pressure for shallow water flow. Computer Methods in Applied Mechanics and Engineering, 178(2), 199–214 (1999)MATHGoogle Scholar
- [6]Wu, X. G., Shen, Y. M., and Wang, M. Research on the vertical 2D modelling of shallow water in σ coordinates with non-hydrostatic pressure assumption (in Chinese). Journal of Hydroelectric Engineering, 24(1), 93–111 (2005)Google Scholar
- [7]Casulli, V. A semi-implicit finite difference method for non-hydrostatic, free-surface flows. Int. J. Numer. Meth. Fluids, 30(4), 425–440 (1999)MATHCrossRefGoogle Scholar
- [8]Yuan, H. L. and Wu, C. H. A two-dimensional vertical non-hydrostatic σ model with an implicit method for free-surface flows. Int. J. Numer. Meth. Fluids, 44, 811–835 (2004)MathSciNetMATHCrossRefGoogle Scholar
- [9]Haney, R. L. On the pressure gradient force over steep topography in σ coordinate ocean models. Journal of Physical Oceangraphy, 21, 610–619 (1991)CrossRefGoogle Scholar
- [10]Stelling, G. and van Kester, J. A. T. M. On the approximation of horizontal gradients in σ coordinates for bathymetry with steep bottom slopes. Int. J. Numer. Meth. Fluids, 18, 915–935 (1994)MATHCrossRefGoogle Scholar
- [11]Stelling, G. and Zijlema, M. An accurate and efficient finite-difference algorithm for nonhydrostatic free-surface flow. Int. J. Numer. Meth. Fluids, 43, 1–23 (2003)MathSciNetMATHCrossRefGoogle Scholar
- [12]Namin, M. M., Lin, B., and Falconer, R. A. An implicit numerical algorithm for solving nonhydrostatic free-surface flow problems. Int. J. Numer. Meth. Fluids, 35, 341–356 (2001)MATHCrossRefGoogle Scholar
- [13]Bergh, J. and Berntsen, J. Numerical studies of wind forced internal waves with a non-hydrostatic model. Ocean Dynamics, 59(6), 1025–1041 (2009)CrossRefGoogle Scholar
- [14]Thomas, L. H. Elliptic Problems in Linear Difference Equations over a Network, Watson Sci. Comput. Lab. Report, Columbia University, New York (1949)Google Scholar
- [15]Orlanski, I. Simple boundary-condition for unbounded hyperbolic flows. J. Comput. Phys., 21(3), 251–269 (1976)MATHCrossRefGoogle Scholar
- [16]Nadaoka, K., Beji, S., and Nakagawa, Y. A fully-dispersive nonlinear wave model and its numerical solutions. Proc. Int. Conf. Coastal Eng. (ed. Billy, L. E.), ASCE, New York, 427–441 (1994)Google Scholar
- [17]Beji, S. and Battjes, J. A. Experimental investigation of wave propagation over a bar. Coastal Eng., 19(2), 151–162 (1993)CrossRefGoogle Scholar
- [18]Bai, Y. F. and Cheung, K. F. Depth-integrated free-surface flow with a two-layer non-hydrostatic formulation. Int. J. Numer. Meth. Fluids, 69, 411–429 (2012)MathSciNetMATHCrossRefGoogle Scholar
- [19]Lin, P. Z. and Li, C. W. A σ-coordinate three-dimensional numerical model for surface wave propagation. Int. J. Numer. Meth. Fluids, 38, 1045–1068 (2002)MATHCrossRefGoogle Scholar
- [20]Zijlema, M. and Stelling, G. Further experiences with computing non-hydrostatic free-surface flows involving water waves. Int. J. Numer. Meth. Fluids, 48, 169–197 (2005)MathSciNetMATHCrossRefGoogle Scholar