Consider the nonresonant traveling forced solution, with and . Put , , where is the mean position of a fluid element. At linear order, evaluate the velocity field at this mean position: substituting into its spatial arguments would change the already first-order velocity only at second order. With , differentiation of the velocity potential givesSince , integration, with zero mean displacements, yieldsIf both coefficients are nonzero, eliminating the wave phase proves that the pathline is an ellipse:Its principal axes of an ellipse are horizontal and vertical, with respective semi-axesThus the full axis lengths are and . The signed coefficients also determine the direction of traversal. The useful checks and reproduce the vertical displacements of the free surface and bottom.
To identify the major axis without comparing the two expressions separately, use :Consequently the major axis is horizontal if and vertical if ; equality gives circles. If or vanishes at a particular depth, the first-order orbit degenerates to a line segment. These are linearized particle orbits of a bottom-forced gravity wave, not exact closed trajectories at all orders: a higher-order calculation may introduce a mean drift.
Principal axes of an ellipse 2026-10-31
The principal axes of an ellipse are the two perpendicular symmetry axes through its center of an ellipse. For a symmetric positive-definite matrix , its orthonormal eigenvectors give those directions and its positive eigenvalues give semiaxis lengths . This follows by orthogonal diagonalization of the defining quadratic form. In , the axes are already horizontal and vertical, with semiaxes and full lengths . Equal semiaxes give a circle, for which every perpendicular pair through the center can serve.
