The vigor of convection is measured by the Rayleigh number (Ra). These movies show the effect
on increasing the Rayleigh number of a fluid of constant viscosity (isoviscous). Some of the lower
Rayleigh number examples don't have movies because they are not time-dependent (they have constant
flow patterns with time).
Minerals that compose the Earth's mantle have a temperature-dependent viscosity, meaning
that they flow more easily if they are hot than if they are cold. The following movies
all have a Raleigh number of 106, but they differ in the temperature-dependence
of viscosity. The viscosity contrast indicates how much the viscosity changes from the hottest
to the coldest regions of the model.