With the help of these lines, parameters such as cloud condensation level, level of free convection, onset of cloud formation.

Due to the subsidence within this type of system, a cap can be set up which inhibits the development of free convection.

Finally, the LCL can also be considered in relation to the level of free convection (LFC).

These cover laminar secondary flows, turbulent flows, free convection and particle motion and deformation.

When analyzing potentially mixed convection of a liquid, the Archimedes number parametrizes the relative strength of free and forced convection.

For the first case, the second boundary condition is that there is free convection at the tip.

Heat transfer experiments include free convection, forced convection, composite wall, and heat exchanger apparatus.

Natural convection, or free convection, occurs due to temperature differences which affect the density, and thus relative buoyancy, of the fluid.

It is a very important dimensionless parameter in analyzing natural or free convection.

Natural or free convection is a function of Grashof and Prandtl numbers.