Glider Instructor Practice Test

Convective circulation develops when a vertical loop is completed by cooler, sinking air pulling surrounding air downward, which in turn allows warm air to rise and feed the loop. This sinking of cool air creates the pressure and motion that draw in warmer surface air to replace it, sustaining the updraft. In other words, the downward branch is essential to drive and maintain the upward motion in the center, making this description the best explanation of how a convective cell forms. Note that warm air rising is a component of convection, but focusing only on the rising part misses the need for the cooler air to sink somewhere else to complete the circulation. Condensation can enhance buoyancy and strengthen updrafts, but it isn’t the fundamental driver of the development of the convective loop. Horizontal wind shear affects the organization of convection rather than its basic formation.