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THE POPULAR SCIENCE MONTHLY.
which has taught us that squalls and thundershowers constitute depressions in miniature, or at least weak secondary depressions dependent upon a principal depression and formed under its immediate influence.
The old miller, an observer by virtue of his profession and then an observer by the force of circumstances, was obliged to study the wind in all its manifestations of direction and force; he was thus aware that its maximum velocity corresponded with the maximum temperature of the day. Although this rule is not without exceptions, the miller was rarely mistaken. Proof of this is given in the habitual and reassuring response to the farmers who came to the mill in the afternoon, when the wind had fallen so low that no grinding could be done:
"Come to-morrow noon again,
And then I will grind your grain."
Everyday observation has taught us that things really go thus when the wind originates under anticyclonic conditions; in the opposite case, if the wind rises in the evening and gains force during the night, the meteorologist concludes that its origin is cyclonic, and a change of weather is probable.—Translated for The Popular Science Monthly from Ciel et Terre.