Summary

Portrait of Svante Arrhenius Svante Arrhenius On the Influence of Carbonic Acid in the Air upon the Temperature of the Earth (1897)

As the enormous quantities of carbonic acid (representing a pressure of many atmospheres) that are now fixed in the limestone of the Earth's crust cannot be conceived to have existed in the air but as an insignificant fraction of the whole at any one time since organic life appeared on the globe, and since therefore the consumption through weathering and formation of carbonates must have been compensated by means of continuous supply, we must regard volcanic exhalations as the chief source of carbonic acid for the atmosphere.
Source: Wikisource

Portrait of Svante Arrhenius Svante Arrhenius On the Influence of Carbonic Acid in the Air upon the Temperature of the Earth (1897)

The selective diffusion is extraordinarily great for the ultra-violet rays, and diminishes continuously with increasing wave-length of the light, so that it is insensible for the rays that form the chief part of the radiation from a body of the mean temperature of the Earth.
The selective absorption of the atmosphere is * * * of a wholly different kind. It is not exerted by the chief mass of the air, but in a high degree by aqueous vapor and carbonic acid, which are present in the air in small quantities.
Source: Wikisource

Portrait of Svante Arrhenius Svante Arrhenius On the Influence of Carbonic Acid in the Air upon the Temperature of the Earth (1897)

In the Physical Society of Stockholm there have been occasionally very lively discussions on the probable causes of the ice age; and these discussions have, in my opinion, led to the conclusion that there exists as yet no satisfactory hypothesis that could explain how the climatic conditions for an ice age could be realized in so short a time as that which has elapsed from the days of the glacial epoch. The common view hitherto has been that the Earth has cooled in the lapse of time
Source: Wikisource

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