Note.-The following very brief and inadequate notice of an important paper presented to the Royal Swedish Academy of Sciences in December, 1895, and printed in the Philosophical Magazine, Volume XLI, pages 237-276, is given here chiefly for the purpose of directing attention to an entirely novel and simple explanation of the vexed questions relating to the Earth's temperature in past times and to the cause of the Glacial Epoch.It is impossible in the present place to give more than the shortest abstract.-E.S. H.
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Svante Arrhénius (1897) studied this question.
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