Order the stages in the development of a thunderstorm in the order in which they occur from top to bottom. Falling precipitation cools the air around it, forming downdrafts. That updrafts cease, and precipitation stops. Equal amounts of updrafts and downdrafts form convection cells. Warm, moist air rises quickly, and the moisture condenses into a visible cloud. Then updrafts form. The updrafts slow as downdrafts decrease the supply of warm, moist surface air. Precipitation begins to fall.

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Social Studies

Karsyn Little

6 July, 17:37

Order the stages in the development of a thunderstorm in the order in which they occur from top to bottom. Falling precipitation cools the air around it, forming downdrafts. That updrafts cease, and precipitation stops. Equal amounts of updrafts and downdrafts form convection cells. Warm, moist air rises quickly, and the moisture condenses into a visible cloud. Then updrafts form. The updrafts slow as downdrafts decrease the supply of warm, moist surface air. Precipitation begins to fall.

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Jerimiah Day · Answer 1

warm moist air rises quickly, the moisture condenses into a visible cloud. the updrafts form. precipitation begins to fall. falling precipitation cools the air around it, for ing downdrafts. equal amounts of updrafts and downdrafts form convection cells. the updrafts slow as downdrafts decrease the supply of warm, moist surface air. the updrafts cease and precipitation stops.

Explanation:

A thunderstorm is a phenomenon of nature that causes an extremely violent rain, with strong winds and large amounts of water; it may even be accompanied by lightning, hail, lightning and thunder.

A thunderstorm, usually originates in clouds called cumulonimbus and occurs in the following order:

warm moist air rises quickly, the moisture condenses into a visible cloud. the updrafts form. precipitation begins to fall. falling precipitation cools the air around it, for ing downdrafts. equal amounts of updrafts and downdrafts form convection cells. the updrafts slow as downdrafts decrease the supply of warm, moist surface air. the updrafts cease and precipitation stops.