20/09/2022
Lightning generates from inside the cold regions of a cloud.
Inside each cloud is an ice cold part around -15°C to -25°C, which causes much of the water in the clouds to turn into tiny ice crystals. The powerful updrafts of high altitudes blow these crystals upwards, along with small droplets of liquid water. As these particles bounce around and against each other, they each gain a small static charge which adds up between them.
Typically, the upper part of a cloud will gain a positive charge, while the middle and lower parts of a cloud gain a negative charge. While the actual process remains unclear, lightning erupts once the charge becomes too much. The excess static crosses over from one side to the other as lightning, neutralizing itself in the process.
Scientists still aren’t sure about what draws lightning to the ground.
All they know is that channels of ionized air called ‘leaders’ slowly descend from the clouds to the Earth’s surface. Forming step-like formations of ionized air as they descend, these channels occur in different levels.
When lightning strikes downward, they follow these channels, which gives lightning its distinctive arcing pattern instead of a straight line. How’s that for intriguing lightning facts?
Lightning does not have heat.
When lightning comes down, it heats up the air it passes through up to 50,000 Kelvin, which makes it hotter than the Sun’s surface at 5,778 Kelvin. The heat of the air also gives lightning its bright and distinctive blue-white color, with the human eye perceiving that heat as colored light.
Despite reacting with the air, lightning itself does not possess an innate heat. With each lightning strike, the air around it cools in a matter of milliseconds.