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" Rarifaction made by his greatest Meridian Heat, is with him carried Westward, and consequently the tendency of the whole Body of the lower Air is that way. "
The Nautical Magazine: A Journal of Papers on Subjects Connected with ... - Page 534
1835
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Miscellanea Curiosa: Being a Collection of Some of the Principal Phaenomena ...

Royal Society (Great Britain) - 1705 - 398 pages
...the Rarifaftion made by his greateft Meridian Heat, is with him carried Weftward, and confequently the tendency of the whole Body of the lower Air is that way. Thus a general Eafterly Wind is formed, which being imprefled upon all the Air of a vail Ocean, the...
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Miscellanea Curiosa: Containing a Collection of Some of the ..., Volume 1

Edmond Halley, Richard Mead - 1708 - 430 pages
...the Rarifaction made by his greateft Meridian Heat, is with him carried Weftward, and confequently the tendency of the* whole Body of the lower Air is that way. Thus a general Eafterly Wind is formed, which being imprefled upon all the Air of a vaft Ocean, the...
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Philosophical Transactions and Collections, to the End of the Year ..., Volume 2

Royal Society (Great Britain) - 1722 - 956 pages
...the Rarefaction made by his greatcil Meridian Heat, is with him carried Weftward, and confequcntly the Tendency of the whole Body of the lower Air is that way. Thus a General Eaiterly Wind is formed, which being impreiTed upon all the Air of a vaft Ocean, the...
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An Exact Survey of the Tide: Explicating Its Production and Propagation ...

Edward Barlow - 1722 - 426 pages
...refaction made' by his greateft Meridian Heat, is, with him, carried Wejtward ; and confequently, ther Tendency of the whole Body of the lower Air is that way : Hence is formed a general Eafterly Wind • which being imprefid upon all the Air of a. vaft O'cean,...
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The Gardeners and Florists Dictionary, Or a Complete System of Horticulture ...

Philip Miller - 1724 - 504 pages
...agreeable to the known Properties of the teft Meridian Heat is with him carried wefluiard, and confequently the tendency of the whole Body of the lower Air is that Way, Thus a general eaflerly Wind is formed, which being impreffed upon all the Air of a vaft Ocean, the...
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The Philosophical Grammar: Being a View of the Present State of Experimented ...

Benjamin Martin - 1755 - 386 pages
...the Rarifaclion made by his greateft meridian Heat, is with him carried Wejlward ; and confequently, the Tendency of the whole Body of the lower Air is that Way : And thus a general TLaJl-Wind is formed in the Atlantic and great South Sea, perpetually blowing...
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The Christian Philosopher: A Collection of the Best Discoveries in Nature ...

Cotton Mather - 1815 - 378 pages
...to an equilibrium. The presence of the sun also continually shifting to the westward, that part to which the air tends, by reason of the rarefaction...tendency of the whole body of the lower air is that way. Thus a general easterly wind is formed. From this principle, the easterly wind on the north side of...
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The London encyclopaedia, or, Universal dictionary of ..., Part 2, Volume 17

Thomas Curtis (of Grove house sch, Islington) - 426 pages
...which are more rarefied, and less ponderous, to bring it to an equilibrium ; also, the presence of the sun continually shifting to the westward, that part...tendency of the whole body of the lower air is that way. 178. Thus a general easterly wind is formed, which being impressed upon the air of a vast ocean, the...
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A Complete Epitome of Practical Navigation ...

John William Norie - 1852 - 844 pages
...continually shifting to the westward, that part towards which the air tends, by reason of the rarefaction, is with him carried westward, and consequently the tendency of the whole body of air is that ' wind in the southern hemisphere. 16 whole surface of the globe were sea, these winds...
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The Winds and Their Story of the World

William Leighton Jordan - 1877 - 124 pages
...continually shifting to the westward, that part towards which the air tends, by reason of the rarefaction, is with him carried westward, and consequently the tendency of the whole body of air is that way, hence a general easterly wind is formed, which, being impressed upon all the air of...
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