Constant vorticity water waves in the two-layer geophysical flows with centripetal forces
摘要
We study the dynamical behavior of geophysical water waves with centripetal forces in a two-layer model, with constant and parallel vorticity vectors in the f-plane approximation. For the time-dependent case, under some appropriate regularity conditions on the interface, we show that the bounded flow solutions are actually two-dimensional. For the time-independent case, we consider steady geophysical waves propagating in the x-axis as well as steady geophysical waves propagating in the xy-plane. In both cases, under some assumptions of boundedness and regularity, we prove the two-dimensionality for geophysical flows and geophysical-capillary flows with centripetal forces. In particular, for the steady case in the x-direction, we can further determine some flow solutions with parallel constant vorticity.