Warm climate

Definition and stakes

Philip Lake and Howard Knox and W. A. B. Coolidge,  1911 Encyclopædia Britannica (1911)

“ Climate.—It is well known that as we rise from the sea-level into the upper regions of the atmosphere the temperature decreases. The effect of mountain-chains on prevailing winds is to carry warm air belonging to the lower region into an upper zone, where it expands in volume at the cost of a proportionate loss of heat, often accompanied by the precipitation of moisture in the form of snow or rain. ”
Source: Wikisource

Homer Greene,  Coal and the coal mines (1889)

“ The air was laden with carbon, which is the principal food for plants; so laden, indeed, that man, who is eminently an oxygen-breathing animal, could not have lived in it. The great humidity of the atmosphere was another element favorable to growth. Vegetation never lacked for an abundance of moisture either at root or leaf. Then, too, the climate was universally warm. Over the entire surface of the earth the heat was greater than it is to-day at the torrid zone. ”
Source: Gutenberg

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