The thicknesses of these boundary layers are of the same order because the relevant speeds of convection are the same for both.
The book is broad in scope, bringing in such aspects as the constraints of seismic topography, and mantle convection in other planetary bodies.
Transient uplift is probably generated by temporal and spatial variations in mantle convection.
This minimizes convection of points that leads to uneven node point distributions and is a principal cause of numerical difficulties.
For example, the observed trends for energy transport in a round free jet flow is by the large-scale convection motions.
The large-scale motions transport by simple convection of fluid packets while there is smaller scale transport by gradient diffusion.
We describe experiments on convection in binary fluid mixtures in a large-aspectratio annular container.
This article describes experimental work on the mixed convection regime with flow normal to electrically heated cylinders.
