Abstract
A FAIR idea of the larger fluctuations of a given meteorological element may be had by means of a two-fold smoothing process, e.g. adding the series of values in groups of five (1 to 5, 2 to 6, 3 to 7, &c.), and then doing the same with those sums. In each case the sum is put opposite the middle member of the group.
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MACDOWALL, A. A Relation between Spring and Summer. Nature 72, 56 (1905). https://doi.org/10.1038/072056a0
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DOI: https://doi.org/10.1038/072056a0
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