Titlebook: Nonlinear Physical Oceanography; A Dynamical Systems Henk A. Dijkstra Book 2000 Springer Science+Business Media Dordrecht 2000 Atlantic Oc

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Numerical Techniques,cation points. As will become clear in this chapter, the detail of the dynamical behavior which can be analysed depends on the dimension, say TV, of the dynamical system. For systems of ordinary differential equations of small dimension (. < 10), the origin of very complex spatial/temporal dynamics

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The Wind-Driven Ocean Circulation,ion on time scales from several months to several years. Focus in this chapter is on the North Atlantic ocean circulation, and in particular the Gulf Stream region, since for this region relatively many observations are available. The midlatitude surface ocean circulation has also been extensively s

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1383-8601 e the dynamics of the Gulf Stream in the Atlantic Ocean,the stability of the thermohaline circulation and the ElNiño/Southern Oscillation phenomenon in the Tropical Pacific.On the other hand, the book also deals with the numerical methods forapplying bifurcation analysis on large dimensional dynamic

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