When lightning strikes the Earth, it consists of more than one electrical discharge. These electrical discharges are called stroke. The brilliant flash of light that is seen in a flash of lightning is called a return stroke. These return strokes travel at about the same speed as that of light (that is, approximately 299, 792 kilometres per second).
A distinctive flash of lightning involves a likely difference between the cloud and the ground. This potential difference in the voltage between the cloud and the ground could be to the tune of several hundred million volts. The peak currents are of the order of about 20, 000 amperes. The temperatures in the channels reach upto a maximum of about 30, 000 Kelvin. Air is heated instantly when an electrical charge of lightning passes through it. The heat either causes the molecules of air to expand or to fly out in all directions.
A distinctive flash of lightning involves a likely difference between the cloud and the ground. This potential difference in the voltage between the cloud and the ground could be to the tune of several hundred million volts. The peak currents are of the order of about 20, 000 amperes. The temperatures in the channels reach upto a maximum of about 30, 000 Kelvin. Air is heated instantly when an electrical charge of lightning passes through it. The heat either causes the molecules of air to expand or to fly out in all directions.