two layer non-hydrostatic, staggered momentum conservative, predictor-corrector.
In this Doctoral Thesis, an efficient two layer non-hydrostatic conservative numerical model is constructed to allow the nonlinearity and dispersion effect in the modeling of waves propagation. Stelling and Zijlema (2003) have shown that two layer approximation is adequate for relatively short wa...
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Format: | Dissertations |
Language: | Indonesia |
Subjects: | |
Online Access: | https://digilib.itb.ac.id/gdl/view/33515 |
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Institution: | Institut Teknologi Bandung |
Language: | Indonesia |
Summary: | In this Doctoral Thesis, an efficient two layer non-hydrostatic conservative
numerical model is constructed to allow the nonlinearity and dispersion effect in
the modeling of waves propagation. Stelling and Zijlema (2003) have shown that
two layer approximation is adequate for relatively short waves and the performance
of two layer model is discussed in detail. Here, we implement a slightly different
two layer approach that is more efficient in the case of calculating the pressure
matrix. However, this new two layer approach’s result is comparable with the two
layer model of Stelling and Zijlema (2003).
We implement our two-layer non-hydrostatic scheme for studying two other topics
: the first is gravity waves over a submerged porous media and the second one
is internal waves. The resulting model is validated with the existing analytical
solutions and experimental data. In all cases, the results are satisfactory in the
comparison with analytical and/or experimental results. Furthermore, the model is
subsequently expanded into a 3D model which is validated with a 3D version of
the oscillating basin and verified with the Berkhoff shoal which includes shoaling,
refraction and diffraction of waves. It can be concluded that our two-layer non-
hydrostatic model can indeed be an efficient way to incorporate nonlinearity and
frequency dispersion. Moreover, our two-layer is much faster in the computation
that we need for describing waves propagation toward the shore. |
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