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Updated: May 10, 2025
The distribution of thunderstorms is as yet not well understood, but it appears in many cases that they are attendants on the advancing face of cyclones and hurricanes, the area in front of these great whirlstorms being subjected to the condensation and irregular air movements which lead to the development of much electrical energy.
Sultry, close weather, that sometimes lasts for several days, would also be impossible on the assumption that air rises as soon as it is heated. This explanation supplies us with the force that is necessary to drive the air with the great velocity with which it moves in whirlstorms.
There is a gradual passage, from the small dust eddies, through larger whirlstorms such as that at Lough Neagh, to tornadoes and the largest cyclone; every step of the gradation might be verified by numerous examples; and if this book were a treatise on meteorology, it might be admissible to give them; but to do this would take up too much of my space, and I shall only now make some observations on the largest form of whirlstorm the dreaded cyclone.
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