Two-dimensionality of gravity water flows governed by the equatorial \(f\)-plane approximation (Q1681839)
From MaRDI portal
| This is the item page for this Wikibase entity, intended for internal use and editing purposes. Please use this page instead for the normal view: Two-dimensionality of gravity water flows governed by the equatorial \(f\)-plane approximation |
scientific article; zbMATH DE number 6812673
| Language | Label | Description | Also known as |
|---|---|---|---|
| English | Two-dimensionality of gravity water flows governed by the equatorial \(f\)-plane approximation |
scientific article; zbMATH DE number 6812673 |
Statements
Two-dimensionality of gravity water flows governed by the equatorial \(f\)-plane approximation (English)
0 references
24 November 2017
0 references
The purpose of this paper is to study the system of governing equations for gravity wave trains at the free surface, governed by the equatorial \(f\)-plane approximation. This system consists of seven equations. Choose a rotating coordinate system with origin at a point on the Earth's surface, with the \(x\)-axis pointing to the east, the \(y\)-axis pointing to the north, and the \(z\)-axis pointing upward. The main theorem states that the water flow over this flat bed governed by the first five equations has a constant vorticity only if the flow is two-dimensional. The proof by contradiction, which uses the Phragmen-Lindelöf method, is made by showing a lack of \(y\)-dependence for the velocity field.
0 references
\(f\)-plane approximation
0 references
vorticity
0 references
gravity wave trains
0 references
0 references
0 references
0.8941234
0 references
0.86478376
0 references
0.86309695
0 references
0.8609512
0 references
0.8578926
0 references
0.8556919
0 references
0.85510325
0 references
0.85384357
0 references
0.85321903
0 references