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under a Creative Commons License. Nonlinear Processes in Geophysics Topographic instability of flow in a rotating fluid

By K. I. Patarashvili, Z. J. Tsakadze, M. V. Kalashnik, V. O. Kakhiani, R. J. Chanishvili, J. I. Nanobashvili and M. A. Zhvania

Abstract

Abstract. Here are presented the results of experimental and theoretical studies on a stability of zonal geostrophic flows in the rotating layer of the shallow water. In the experiments, a special apparatus by Abastumani Astrophysical Observatory Georgian Academy of Science was used. This apparatus represents a paraboloid of rotation, which can be set in a regulable rotation around the vertical axis. Maximal diameter of the paraboloid is 1.2 m, radius of curvature in the pole is 0.698 m. In the paraboloid, water spreads on walls as a layer uniform on height under the period of rotation 1.677 s. Against a background of the rotating fluid, the zonal flows are formed by the source-sink system. It consists of two concentric circular perforations on the paraboloid bottom (width is 0.3 cm, radiuses are 8.4 and 57.3 cm, respectively); water can be pumped through them with various velocities and in all directions

Year: 2013
OAI identifier: oai:CiteSeerX.psu:10.1.1.371.1869
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