Dec 1892
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1892natur..47..150c&link_type=abstract
Nature, Volume 47, Issue 1207, pp. 150-151 (1892).
Physics
Scientific paper
AFTER explaining that by ``sunshine'' I intend that which would fall upon the earth if there were no atmospheric obstruction, one must first notice the very elementary truth that the amount of such sunshine at any assumed time and place is in proportion to the altitude of the sun at noon, and also the length of the day. Except at the time of the equinox,the gradual lengthening or shortening of the day, as the solstice is approached, most materially affects, especially in the higher latitudes, the total amount of sunshine received in twenty-four hours.
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