Titlebook: Irreversible Phenomena and Dynamical Systems Analysis in Geosciences; C. Nicolis,G. Nicolis Book 1987 D. Reidel Publishing Company, Dordre

Exterior

Universal Power Spectra for Wave Turbulence; Applications to Wind Waves and 1/f Noiseonlinear order one obtains the results of weak wave turbulence theory. At infinite nonlinear order the power spectrum accumulates at 1/f noise for non-dispersive waves and 1/ω. noise for deep water waves. Effects resulting from a renormalization of the phase velocity are also discussed.

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The Blocking Transitionby Charney and DeVore (1979) that these grosswetterlagen are linked to the existence of multiple equilibria of the dynamic equations underlying the large-scale flow. Transitions between grosswetterlagen can be seen as a consequence of instabilities of these equilibria. Work on this topic is reviewed

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Foreshadow

J. F. Nyem their vacuum values to the bulk values. We recognise three ill-defined regions (in the sense that their edges are not sharp), which are important in determining the optical response of a surface: I the vacuum region; II the (narrow) selvedge region; HI the bulk. Since the advent of modern surface