A+ Ball Lightening.
Streak
When lightning appears in the remote distance and produces little to no thunder, it is often referred to as "heat lightning." This phenomenon occurs when the light from distant lightning strikes travels to the observer without the accompanying thunder, which dissipates over long distances. Heat lightning is typically seen on warm summer nights and is a common misperception that it's a different type of lightning.
When lightning appears as more than one line, it is called "forked lightning" or "branching lightning." This phenomenon occurs when the electrical discharge takes multiple paths as it travels through the atmosphere, creating a jagged appearance. Each branch represents a different path the electrical current has taken as it seeks the ground.
When lightning appears in the distance without accompanying thunder, it is referred to as "heat lightning." This phenomenon occurs when the lightning bolt is too far away for the sound of thunder to be heard, typically beyond 10 miles. The light from the flash can still be visible, especially on warm summer nights, giving the impression of lightning without any audible thunder.
When lightning appears in the remote distance without producing a thunder sound, it is often referred to as "heat lightning." This phenomenon occurs when the lightning is too far away for the sound of thunder to reach the observer, typically occurring during warm summer evenings. The light from the lightning can still be seen, but the absence of thunder indicates that the storm is not directly overhead.
Ball lightning. It is a rare phenomenon where a small, glowing sphere appears during thunderstorms. This type of lightning is not well understood and can vary in size and color.
When lightning appears as small bursts in a dotted line, it is called sheet lightning. This type of lightning is caused by distant lightning flashes reflecting off clouds or atmospheric particles, creating a diffuse illumination in the sky.
Streak
A type of lightning that appears as a single long line is called a "fork lightning" or "bolt from the blue." It often occurs when lightning strikes horizontally within a cloud or between clouds rather than toward the ground.
When lightning appears as more than one line, it is called forked lightning. This occurs when the electrical discharge in the atmosphere branches out into multiple paths as it travels from the cloud to the ground. Forked lightning can create a striking visual display during a thunderstorm.
A+ Beaded Lightning
When lightning appears in the remote distance and produces little to no thunder, it is often referred to as "heat lightning." This phenomenon occurs when the light from distant lightning strikes travels to the observer without the accompanying thunder, which dissipates over long distances. Heat lightning is typically seen on warm summer nights and is a common misperception that it's a different type of lightning.
When lightning appears as more than one line, it is called "forked lightning" or "branching lightning." This phenomenon occurs when the electrical discharge takes multiple paths as it travels through the atmosphere, creating a jagged appearance. Each branch represents a different path the electrical current has taken as it seeks the ground.
When lightning appears in the remote distance without producing a thunder sound, it is often referred to as "heat lightning." This phenomenon occurs when the lightning is too far away for the sound of thunder to reach the observer, typically occurring during warm summer evenings. The light from the lightning can still be seen, but the absence of thunder indicates that the storm is not directly overhead.
When lightning appears in the distance without accompanying thunder, it is referred to as "heat lightning." This phenomenon occurs when the lightning bolt is too far away for the sound of thunder to be heard, typically beyond 10 miles. The light from the flash can still be visible, especially on warm summer nights, giving the impression of lightning without any audible thunder.
When lightning appears in the remote distance and appears to produce no thunder sound, it is popularly known as "heat lightning." Meteorologists will tell you that there really is no such thing as a distinct type of lightning that is not followed by thunder. All lightning produces thunder, but it is only audible for a distance of some 15-20 miles from the storm. At night, lightning can be seen for distances of up to 125 miles if the conditions are right. So when lightning is seen but no thunder is heard, you are simply too far away from the storm.
The colored layer of the sun is known as the chromosphere. It is located above the sun's visible surface (photosphere) and is characterized by its reddish coloration. The chromosphere is also where solar prominences and solar flares occur.