Science

What is White Rainbow?

How does Rainbow occur?

A rainbow is a meteorological weather event in which the colors of the rays created by reflection and refraction of sunlight occur in rain droplets and fog clouds.

When the clouds in the air are in front of the sun, rainbows cannot form.
The sun must be in the sky in order for the rainbow to form or be seen. When the rays formed by the rainbows appear in general, it is the time when rainfall stops in the evening. The rainbows are generally the opposite part of the sun.

Although mostly seen as a semicircular circle, a circle called a rainbow can be seen from a mountain and a high point.

It is formed by the reflection of rainbow light reflections being broken by rain droplets and fog grains. Generations made up of large drops are very bright and the color separation is glaring. The rainbows of small rain droplets can be more delicate and wider. Most commonly seen are the white rainbows, also known as fog belts, formed by fog cloud or mist.

How White Rainbow is Formed

The white rainbow as a whole generally occurs in a foggy environment and can be named separately as a fog belt. The fog belts are made up of small water drops. Small drops cannot emit light like big drops that can form a simple rainbow. In general, the important event on this subject is the general longitude of lights of different colors. Due to these weather events, the fog belts lack color scheme. It simply has a red inner edge and a blue inner edge.

It can usually be seen by looking at the air on the surface formed by the clouds, not when there is fog. In order to see this event, you must be looking at the ground very carefully. In general, white rainbows can be seen in the opposite part of the sun. In these weather events, the white rainbow can be seen more rarely than other rainbow species.

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