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Proceedings of the Royal Society of London. A. Mathematical and Physical Sciences, 1987
Thermal convection in a fluid layer is an example of a dynamical system governed by partial differential equations. As the relevant control parameter (the Rayleigh number) is increased, successive bifurcations may lead to chaos and the nature of the transition depends on the spatial structure of the flow.
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Thermal convection in a fluid layer is an example of a dynamical system governed by partial differential equations. As the relevant control parameter (the Rayleigh number) is increased, successive bifurcations may lead to chaos and the nature of the transition depends on the spatial structure of the flow.
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Physics of Mantle Convection [PDF]
, 2007 This chapter presents the fundamental physics necessary to understand the complex fluid dynamics of mantle convection. The first section derives the equations of conservation for mass, momentum and energy, and the boundary and interface conditions for the various physical quantities.
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Could Machine Learning Break the Convection Parameterization Deadlock?
Geophysical Research Letters, 2018G Yacalis +2 more
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Anomalously weak Labrador Sea convection and Atlantic overturning during the past 150 years
Nature, 2018D J R Thornalley +2 more
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Evaluation of the convection-resolving regional climate modeling approach in decade-long simulations
Journal of Geophysical Research D: Atmospheres, 2014Christoph Schär +2 more
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