Key Features:
- Provides a complete, concise dynamical picture of the hydromagnetic dynamo process generated by non-equilibrium turbulence.
- Emphasizes the role of non-diffusive large-scale dynamo mechanisms
- Provides a possible natural interpretation of the phenomenon of magnetic excursions and reversals in natural systems, such as the Earth, through the non-equilibrium dynamo mechanism, which leads to long-term oscillations of turbulent transport coefficients.
- Emphasizes the existence of a variety of distinct dynamical effects leading to mean-field dynamo in fully developed, strongly nonlinear turbulence.
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