Convective lifting is due to vertical instability. Convective current will form in order to transport the building heat energy at the surface upwards and to bring down cooler air aloft.
The four types of atmospheric lifting mechanisms are orographic lifting, frontal lifting, convergence lifting, and convectional lifting. Orographic lifting occurs when air is forced to rise over a mountain range. Frontal lifting happens at the boundary of two air masses with different temperatures and densities. Convergence lifting occurs when air flows together and is forced to rise. Convectional lifting is the result of surface heating causing air to rise.
The 4 lifting mechanisms that make air rise are orographic lifting (when air is forced upward by a mountain or slope), frontal lifting (when warmer, less dense air is forced over cooler, denser air), convergence lifting (when air flows together and is forced to rise) and convectional lifting (when air is heated and rises due to its reduced density).
The flux control method is the convectional and the non-convectional method of speed control of an induction motor.
Convectional currents would be a topic in fluid flows
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Tropical
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Convectional Precipitation
pyroclastic and convectional.
Equatorial regions experience convectional rainfall because of the intense heating of the sun, which warms the air near the surface. This warm air rises rapidly, cools, condenses, and forms clouds that lead to heavy rainfall. The constant heating and rising of warm, moist air in these regions create a cycle of convectional rainfall.
Convectional rainfall
any war where there are no troops used.