Publications

In this paper, we study fluid dynamics taking into account two effects governing fluid’s motion, an external one caused by Earth’s rotation: Coriolis effect, besides an internal effect, caused by the interaction between fluid’s molecules: the surface tension. So a new physical frame is considered here. At first, we will derive formally a new model of equations describing the motion in Camassa–Holm regime. Furthermore, large-time local well-posedness of the main model will be investigated in H^s(R^n) for s>3/2.