Field-change due to lightning flashes is recorded by using simultaneously an electric fluxmeter and an amplifier oscillograph of WATSONWATT and APPLETON'S type. At the same time, time-variation of the illumination of the whole sky due to flashes is recorded by means of photomultipliers and a cathode-ray oscillograph.
In case of flashes to the ground, they emit weak light continuously during their leader processes, while their return strokes are observed as instant and brightest bursts of light. Throughout the periods between and after the strokes, a number of fairly bright bursts of light having the duration of 1 to 2 m-sec occur successively at th e intervals of about 4 to 30 m-sec.
In case of cloud flash e s, fairly bright bursts occur similarly throughout their whole duration. When the field-change of the leader type is recorded in a part of their duration, weak and continuous luminosity is observed in accordance with this field-change. These bright bursts of light observed both in flashes to the ground and in cloud flashes are caused by discharge processes which produce small rapid field-changes named K-change by one of the authors.
It has been made clear that in the discharge pr o cess of this type, the brighter burst of light is associated with the discharge process in which the rate and the frequency of the current change are higher.
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