A numerical model was used to simulate the propagation of internal waves (IW) along the surface layer. The results show that strong water exchange during IW propagation results in strong free surface flow and produces small but distinct free surface waves. We found a close relationship between the internal and ocean surface waves. Our intuitive reaction is that by training the relationship between the water surface wave height and the internal wave waveform, the internal wave waveform can be reversed from the water surface wave height value. This paper intends to validate our intuition. The artificial neural network (ANN) method was used to train the Fluent simulated results, and then the trained ANN model was used to predict the inner wave...
The height of a wave at the time of its breaking, as well as the depth of water in which it breaks, ...
AbstractThe prediction of solitary wave run-up has important practical significance in coastal and o...
The theory of three distinct problems arising in geophysical fluid dynamics is considered. Part I co...
Nonlinear permanent progressive wave is one of the most important applications in water waves. In th...
Abstract: This paper presents an overview of the development of the numerical wave prediction models...
Wave propagation around and inside a harbor is conventionally studied by numerically solving a repre...
textInternal waves are generated in the ocean by oscillating tidal flow over bottom topography such ...
The physical process of generation of waves by wind is extremely complex, uncertain and not yet full...
Ocean surface wave environment due to its randomness has mostly been analyzed and understood from a ...
Sound can travel long distances through the deep ocean due to a naturally formed waveguide. Internal...
The objective of this paper is to use an artificial neural network (ANN) model to train the output o...
Information on heights of waves and their distribution around harbor entrances is traditionally obta...
Our long-term goal is to employ numerical simulation to generate accurate predictions of the nature ...
Two surface waves can interact to produce an internal gravity wave by nonlinear resonant coupling. T...
Internal waves are complex phenomena which occur uniquely in fluids which are stratified, or have va...
The height of a wave at the time of its breaking, as well as the depth of water in which it breaks, ...
AbstractThe prediction of solitary wave run-up has important practical significance in coastal and o...
The theory of three distinct problems arising in geophysical fluid dynamics is considered. Part I co...
Nonlinear permanent progressive wave is one of the most important applications in water waves. In th...
Abstract: This paper presents an overview of the development of the numerical wave prediction models...
Wave propagation around and inside a harbor is conventionally studied by numerically solving a repre...
textInternal waves are generated in the ocean by oscillating tidal flow over bottom topography such ...
The physical process of generation of waves by wind is extremely complex, uncertain and not yet full...
Ocean surface wave environment due to its randomness has mostly been analyzed and understood from a ...
Sound can travel long distances through the deep ocean due to a naturally formed waveguide. Internal...
The objective of this paper is to use an artificial neural network (ANN) model to train the output o...
Information on heights of waves and their distribution around harbor entrances is traditionally obta...
Our long-term goal is to employ numerical simulation to generate accurate predictions of the nature ...
Two surface waves can interact to produce an internal gravity wave by nonlinear resonant coupling. T...
Internal waves are complex phenomena which occur uniquely in fluids which are stratified, or have va...
The height of a wave at the time of its breaking, as well as the depth of water in which it breaks, ...
AbstractThe prediction of solitary wave run-up has important practical significance in coastal and o...
The theory of three distinct problems arising in geophysical fluid dynamics is considered. Part I co...