Then there is consequent non-linearity, and heat flow can develop into phases of convective circulation.
2.
The convective circulation drives up-wellings and down-wellings in Earth's mantle that are reflected in local surface levels.
3.
The layer of convective circulation takes place ) and may be more significant for thermal mixing than normal convection, transporting moist air vertically above the convection boundary.
4.
Available data does not lend to the quantification of the volume transports associated with this western boundary region, or to the determination of deep convective circulation along the western boundary.
5.
Nevertheless, if the wall between the system and its surroundings is thick and contains fluid, in the presence of a gravitational field, convective circulation within the wall can be considered as indirectly mediating transfer of energy as heat between the system and its surroundings, though they are not in direct contact.
6.
This is conceptually different from transfer of energy as heat through a thick fluid-filled wall in the presence of a gravitational field, between a closed system and its surroundings; in this case there may convective circulation within the wall but the process may still be considered as transfer of energy as heat between the system and its surroundings; if the whole wall is moved by the application of force from the surroundings, without change of volume of the wall, so as to change the volume of the system, then it is also at the same time transferring energy as work.
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