“…The experimental data obtained by Orville (1968a) on the temperature of the lightning stepped leader channel show that at the formation of the step the channel temperature increases to about 25,000-30,000 K. Subsequently, the temperature decreases to about 15,000 K and remains at that level until the channel is retraced by the return stroke. The theoretical calculations of Paxton et al (1986), Hill (1971) and Plooster (1971) also indicate that by the time the pressure inside the spark channel reduces to the atmospheric pressure the average temperature in the channel is close to 20,000-15,000 K. After the pressure equilibrium is reached, the cooling of the channel takes place mainly due to the entrainment of cold air across the channel boundaries into the hot core of the channel effectively reducing the diameter of the hot core (Hill et al, 1980). Similarly, Eq.…”