How to draw a thunderstorm in Grade Two?

How to draw a secondary thunderstorm, the example is as follows:

First, draw clouds with black strokes on white paper; Then draw lightning; Then draw the raindrop part; When finished, paint the lightning yellow; Dark clouds are shaded; The stick figure of Thunderstorm is completed.

Extended data:

Lei is a commonly used Chinese word, pronounced léi, which was first seen in Oracle Bone Inscriptions. Its original meaning is the powerful sound released by the discharge when two clouds with opposite electrical properties approach. Shuowen: "technetium is weak in yin and yang, and thunderstorm creatures are also." Later, it was extended to thunder and was quickly compared to thunder; It can also express thunderous sounds.

Thunderstorm is a kind of shower phenomenon accompanied by lightning. Produced under thunderstorm cumulonimbus clouds. It is characterized by large-scale cloud movement, which is much more violent than showers and accompanied by discharge, and is common in summer. When showers come, there are often strong winds and thunderstorms. Persistent and intense thunderstorms can often reach the level of heavy rain.

In summer, direct sunlight makes the water on the ground evaporate faster than in winter, spring and autumn. The air close to the ground can receive more water vapor because of its high temperature, which leads to the decrease of air density, the lightening of air and the rising of the lightened air.

With the increase of altitude, the temperature will gradually drop (0.6 degrees per 100 meters), and the air will gradually cool down. When the air is cool, it can't hold the original abundant water vapor. Some water vapor will condense into small water droplets, and the sky will be cloudy. This is a cumulonimbus cloud.

When the small water droplets in the cumulonimbus cloud constantly collide and merge into larger water droplets, they begin to fall, while the hot air rising from the ground keeps rushing upwards, and the friction between them is charged. The rising airflow is positively charged and the falling water droplets are negatively charged.

With the passage of time, a large number of positive charges have accumulated at the top of cumulonimbus clouds, while many negative charges have accumulated at the bottom. Due to the negative charge at the bottom of cumulonimbus clouds, the ground is also positively charged.

The water droplets in the cloud merge and increase until the rising hot air can't hold it, and then fall straight from the cloud. The hot air at the lower level was drenched by rain and suddenly became cold. Instead of rushing up, it turned to the ground. At this point, the charge in the air began to discharge, accompanied by thunderous thunder.