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Symmetry-breaking-induced rare fluctuations in a time-delay dynamic system
Yin Wang1,2, Wei Xu1, Pik-Yin Lai3
1Department of Physics, Hong Kong University of Science and Technology, Clear Water Bay, Kowloon, Hong Kong.
This study investigates dynamic instabilities in turbulent Rayleigh-Bénard convection using coupled nonlinear delay differential equations. Findings reveal chaotic solutions with large fluctuations, explaining massive thermal plume eruptions and circulation reversals in geophysical systems.
Area of Science:
- Fluid Dynamics
- Nonlinear Dynamics
- Geophysics and Astrophysics
Background:
- Turbulent Rayleigh-Bénard convection exhibits complex dynamics, including boundary layer oscillations.
- Massive thermal plume eruptions and circulation reversals are observed in geophysical and astrophysical convection systems.
Purpose of the Study:
- To model dynamic instabilities in coupled nonlinear delay differential equations for turbulent Rayleigh-Bénard convection.
- To understand the origin of rare massive eruptions and flow pattern changes in convection systems.
Main Methods:
- Analysis of two coupled nonlinear delay differential equations.
- Introduction of sensitivity parameters for top and bottom boundary layer instabilities.
- Identification of in-phase single-period, multi-period, and chaotic solutions.
Main Results:
- Three solution types were identified: in-phase single-period oscillations, multi-period oscillations, and chaos.
- Chaotic solutions exhibit rare, large-amplitude fluctuations.
- Statistical properties of fluctuations match experimental observations of thermal plume eruptions.
Conclusions:
- The study provides insights into the mechanisms driving massive thermal plume eruptions.
- The model explains random reversals of large-scale circulation in turbulent convection.
- Findings offer new perspectives on phenomena in geophysical and astrophysical convection systems.
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