Travels In The United States Of America; Commencing In The Year 1793, And Ending In 1797. With The Author's Journals Of His Two Voyages Across The Atlantic By William Priest































































































































































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The middle states of North America are hotter and colder _at intervals_,
not only than England, but than any part - Page 84
Travels In The United States Of America; Commencing In The Year 1793, And Ending In 1797. With The Author's Journals Of His Two Voyages Across The Atlantic By William Priest - Page 84 of 128 - First - Home

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The Middle States Of North America Are Hotter And Colder _At Intervals_, Not Only Than England, But Than Any Part Of The Old Continent, Under The Same Parallel Of Latitude.

Jefferson says, "Our changes from heat to cold are sudden and great.

The mercury in Fahrenheit's thermometer has been known to descend from 92 to 47, in thirteen hours."

And I copied the following from a New York paper: -

"Wednesday, the 14th of May, the mercury in Fahrenheit rose to 91 degrees, The Saturday night following, there was a severe frost. The next Tuesday and Wednesday, the mercury rose to 85 degrees; from the 20th to the 26th, it has been nearly stationary, varying only from 60 to 64.: Easterly wind, and rain."

These violent transitions from heat to cold, are produced by means of the N.W. wind, which in this country is the most keen and severe of any that is to be met with on the face of the globe. It is much the most prevalent wind we have, and seldom fails to blow four or five days with great uniformity. This wind is perfectly _dry_, and so uncommonly penetrating, that I am convinced it would destroy all the plagues of Egypt in a very short time. You may recollect, I informed you of the astonishing effect of this powerful agent in stopping the yellow fever in a few hours, last year, at Baltimore.

Neither the prevalence, nor uncommon severity of this wind has been properly accounted for; but we may now expect something more satisfactory on this subject, from the celebrated Volney; who is here endeavouring to investigate the causes of this, and other phenomena, relative to the winds of this continent.

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