LAUSR

abstract One of the main causes of the formation of internal waves is the ocean currents, from the seabed's mounds. For this reason, numerous empirical studies have been carried out in laboratories on the flow of streams on artificial mounds or the passage of objects in a stratified medium. The purpose of this study is to identify the changes in the density of the layers by internal waves due to the movement of the physical model in a stratified water with different Froude numbers. This study is done in, a large stratified tank that density changes due to movement of spherical and airfoil bodies are recorded by an array of fast response sensors. Lee waves and the blocking area are well illustrated before and after waves, created by passing objects, are transmitted through the tank, and are visualized using optical shadowgraph technique. The results showed that the mean amplitude of waves increases with increasing Froude numbers. The average wave's periods before the object reaches the lowering point of 0.4D/U (D being the thickness of the moving object and U is its speed) and then increases, and the mean period after the arrival of the object decreases with the Froude number.