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ABSTRACT SOME twelve years ago I gave (_Phil. Mag._, March, 1867, “Climate and Time,” p. 548) what appears to be the true explanation of that apparently paradoxical fact observed by Mr.

Glaisher, that the difference of reading between a thermometer exposed to direct sunshine and one shaded _diminishes_, instead of increases, as we ascend in the atmosphere. This led me to an

important conclusion in regard to the influence of aqueous vapour on the melting-point of snow; but recent objections to some of my views convince me that I have not given to that

conclusion the prominence it deserves. I shall now state in a few words the conclusion to which I refer. Access through your institution Buy or subscribe This is a preview of subscription

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ACCESS OPTIONS: * Log in * Learn about institutional subscriptions * Read our FAQs * Contact customer support Authors * JAMES CROLL View author publications You can also search for this

author inPubMed Google Scholar RIGHTS AND PERMISSIONS Reprints and permissions ABOUT THIS ARTICLE CITE THIS ARTICLE CROLL, J. Aqueous Vapour in Relation to Perpetual Snow. _Nature_ 22,

191–192 (1880). https://doi.org/10.1038/022191a0 Download citation * Issue Date: 01 July 1880 * DOI: https://doi.org/10.1038/022191a0 SHARE THIS ARTICLE Anyone you share the following link

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