The Typhoon Kezia and Atmospherics

Abstract

The author proposes the consideration that the main origins of atmospherics are the symbol indicating the degree of disturbances in the conditional instability region, of which he confirmed the frontal type and the air mass type. This is not only justified on physics of the formation of atmospherics, discussing from the view point of electromagnetic waves and atmospheric electricity as well as from the meteorological point of view, but also it is confirmed by the observations actually made for years. In this paper the examples concerning the Typhoon Kezia are given and explained in detail. He found that origins of atmospherics concerning to this typhoon are destributed most frequently on the right hand side of the centre of the typhoon, especially on the perpendicular direction to the course, and they increase slowly with distance from the centre to 400km, accompanying a small peak at 100km, and at 400km they reach maximum, and then decrease rather rapidly to 600km.