Three Stages of Thunderstorm Formation

Types of thunderstorms that produce summer rainfall with three stages of thunderstorm formation are called ordinary thunderstorms or thunderstorms of air masses. As warm moist air rises in an unstable atmosphere, they will form warm air to cool as they go up and it will begin to cool down as it becomes cooler than the surrounding air. In an unstable atmosphere, as the height decreases, the temperature of the surrounding air drops faster than the temperature of the rising warm air. As a result, warm and humid air will always be warmer than the atmosphere and continue to rise to high.

Regardless of type, all thunderstorm goes through three stages. Development stage, maturity stage, and disappearance stage. The average thunderstorm has a diameter of 24 kilometers (15 miles). These three stages, which depends on atmospheric conditions, take an average of 30 minutes to complete. Solar radiation affects the ocean. Warm water from the equator tends to circulate to polar regions, but cold extreme water faces the equator. The surface current is initially determined by the condition of the surface wind. Trade winds blow in the west in the tropics and west winds blow east in mid latitudes. This wind mode stresses the surface of the subtropical ocean with a negative curve in the Northern Hemisphere and vice versa in the Southern Hemisphere. The resulting Sverdrup transport is the equator

First, thunderstorms occur in three stages. These three phases are called the cumulus phase, the maturation phase, and the dissipation phase. The cumulus phase is when warm air rises from the surface of the earth. There are various ways to form an upward flow and a warm wind. The air may be pushed upwards in front of the weather and the boundary separates the air of two different densities. This is the place where warm air and cold air collide. Another way is that the air from the ground is heated from the sun. Heat the air. Then the air will rise to the atmosphere. If warm air is wet or damp, it will condense into cumulus clouds. As long as the warm air from the ground continues to increase, this cloud will continue to grow. The second stage is the maturity stage. When cumulus continues to grow. It will eventually become very big. The water inside is big and heavy. The droplet can become very heavy as it can no longer block them