James Mackintosh, Popular Science Monthly (1875)
“ The ascension of air with a higher sensible temperature would not alone suffice to supply the tremendous power of the cyclone. The difference of temperature, even in extreme eases between lower and higher strata, is wholly insufficient to account for the enormous energy developed by our cyclones of hundreds of miles in diameter. We therefore require another source of power. Nor have we far to seek it. The sun's rays falling upon dry earth heat it, and thus raise the temperature of the air in contact with it. ”
