Some features of chaotization of a pulsating barotropic flow over a seamount with elliptic cross-section

Verfasser / Beitragende:
[Yu. G. Izrailsky, V. F. Kozlov, K. V. Koshel]
Ort, Verlag, Jahr:
2003
Enthalten in:
Russian Journal of Numerical Analysis and Mathematical Modelling, 18/3(2003-06-01), 243-260
Format:
Artikel (online)
ID: 378847805
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245 0 0 |a Some features of chaotization of a pulsating barotropic flow over a seamount with elliptic cross-section  |h [Elektronische Daten]  |c [Yu. G. Izrailsky, V. F. Kozlov, K. V. Koshel] 
520 3 |a We consider a barotropic inviscid model of chaotic advection in a unidirectional pulsating background flow over a seamount of an elliptic form. We numerically study the process of passive tracer transport from the vortex area to the flow-through area, and in particular we give the dependence of evolution of the corresponding Poincaré maps on the frequency and amplitude of incident flow pulsations. We propose an approach to the study of the mechanism and parameters of chaotic advection in open systems with finite trajectories lifetime. It is based on studying the time it takes for tracers to be carried out from the vortex area to the flow-through area. We show the essential impact of the seamount orientation with respect to an incident flow on the rate and scenario of tracers transport from the vortex area. 
540 |a Copyright 2003, Walter de Gruyter 
700 1 |a Izrailsky  |D Yu. G.  |u Institute of Automatics and Control Processes of the Far Eastern Branch of the Russian Academy of Sciences, Vladivostok 690032, Russia  |4 aut 
700 1 |a Kozlov  |D V. F.  |u Pacific Institute of Oceanography of the Far Eastern Branch of the Russian Academy of Sciences, Vladivostok 690032, Russia  |4 aut 
700 1 |a Koshel  |D K. V.  |u Pacific Institute of Oceanography of the Far Eastern Branch of the Russian Academy of Sciences, Vladivostok 690032, Russia  |4 aut 
773 0 |t Russian Journal of Numerical Analysis and Mathematical Modelling  |d Walter de Gruyter  |g 18/3(2003-06-01), 243-260  |x 0927-6467  |q 18:3<243  |1 2003  |2 18  |o rnam 
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