Rhythmodinamics of a great number of quasi - periodical geophysical processes in marine systems is analyzed. Their variability is proposed to be considered as a complex, multimode system of stable oscillations - rhythms. These oscillations - rhythms are considered to interact between themselves on the basis on resonance; their intra - spectral variability has a fractal - wave structure. Such approach might be applied for describing geophysical processes and permits to suggest for this a non-traditional version of their spectral models with the harmonic amplitude modulated on the basis of the intra - spectral variability feature.

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