A three-dimensional long-wave steep-slope equation

A complete three-dimensional long-wave polar–Cartesian equation is developed in the frequency domain. This development employs an auxiliary axis system oriented locally in the bottom gradient direction. The long-wave limit of the two-dimensional polar–Cartesian steep-slope equation is also derived. An approximate explicit expression of the coefficients is developed without restrictions on bed steepness. This is achieved by utilising a rational function approximation of the $\arctan$ function, which arises from the formulation of the vertical profile of the flow parameters. Additionally, long-wave equations in both two and three dimensions are developed in the time domain. Simulations of the long-wave equations are compared with those of the extended shallow-water equation for two-dimensional test cases, as well as for the quasi-three-dimensional scenario of oblique incidence. Our equations exhibit better agreement with the exact solutions in the majority of the test cases.

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Publication Details

Journal
Journal of Fluid Mechanics
Published
2025-04-25
DOI
https://doi.org/10.1017/jfm.2025.303
Primary Topic
Coastal and Marine Dynamics
Type
article
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article

A three-dimensional long-wave steep-slope equation

Rafael Schwartz
Journal of Fluid Mechanics
Coastal and Marine Dynamics
article

A three-dimensional long-wave steep-slope equation

Rafael Schwartz
article en

Abstract

A complete three-dimensional long-wave polar–Cartesian equation is developed in the frequency domain. This development employs an auxiliary axis system oriented locally in the bottom gradient direction. The long-wave limit of the two-dimensional polar–Cartesian steep-slope equation is also derived. An approximate explicit expression of the coefficients is developed without restrictions on bed steepness. This is achieved by utilising a rational function approximation of the $\arctan$ function, which arises from the formulation of the vertical profile of the flow parameters. Additionally, long-wave equations in both two and three dimensions are developed in the time domain. Simulations of the long-wave equations are compared with those of the extended shallow-water equation for two-dimensional test cases, as well as for the quasi-three-dimensional scenario of oblique incidence. Our equations exhibit better agreement with the exact solutions in the majority of the test cases.

Journal of Fluid MechanicsVol. 1009
Ariel University (IL)
Openalex Percentile: Top 89%
Coastal and Marine Dynamics
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