 | Monthly literary register - 1820 - 694 pages
...that their heating powers are nearly in\ the same ratio. According to Sir H. Davy's Theory of Mists, land and water are cooled after sunset in a very different...cooling on the land is limited to the surface, and ii very slowly transmitted into into the interior ; wherens in water the upper stratum, when cooled,... | |
 | 1820 - 856 pages
...powers are nearly in the same ratio. Mitts. — According to Sir H. Davy's Theory of Mists, land j>ml water are cooled after sunset in a very different...water will, therefore, in calm and clear weather, and temperatures above 45° Fahrenheit, be warmer than that of the contiguous land ; and consequently the... | |
 | 1821 - 488 pages
...and in greater proportion as the rky is clearer ; but the land and water are eooled by this operation in a very different manner ; the impression of cooling on the land is limited to the surface and very slowly transmitted to the interior ; whereas, in water above 40 dcg. Fahrenheit, as' soon as the... | |
 | 1821 - 734 pages
...and in greater proportion as the sky is clearer ; but the land and water are cooled by this operation in a very different manner ; the impression of cooling on the land is limited to the surface and very slowly transmitted to the interior ; whereas, in water above 40° Fahrenheit, as soon as the upper... | |
 | 1820 - 486 pages
..."t» -AstV'A t,' c " ' iH.- Sir ti. Davy's Theory of Mists.— According to this emi"lieiit chemist, land and water are cooled after sunset in, a very...the surface, and is very slowly transmitted into the in!teribr ; whereas in water the upper stratum, when cooled, descends, and has its place supplied by... | |
 | 1824 - 628 pages
...and in greater proportions as ihe sky is clear ; but the land and water are cooled by this operation in a very different manner: the impression of cooling on the land is limited to the surface, and very slowly transmitted to the interior ; whereas in water above 45° Fahrenheit, as soon as the upper... | |
 | Charles Frederick Partington - 1828 - 468 pages
...direct attention to Sir Humphrey Davy's elegant and simple theory. According to this eminent chemist, land and water are cooled after sunset in a very different...supplied by warmer water from below. The surface of water will, therefore, in calm and clear weather, and in temperatures above 45° Fahrenheit, be warmer... | |
 | John Ayrton Paris - 1831 - 598 pages
...and in greater proportions as the sky is clearer; but the land and water are cooled by this operation in a very different manner : the impression of cooling on the land is limited to the surface, and very slowly transmitted to the interior ; whereas in water above 45° Fah., as soon as the upper stratum... | |
 | John Ayrton Paris - 1831 - 582 pages
...in greater proportions as the sky is clearer ; but the land and water are cooled by this operation in a very different manner : the impression of cooling on the land is limited to the surface, and very slowly transmitted to the interior ; whereas in water above 45° Fah., as soon as the upper stratum... | |
 | John Davy - 1836 - 436 pages
...in greater proportions as the sky is clearer : but the land and water are cooled by this operation in a very different manner ; the impression of cooling on the land is limited to the surface, and very slowly transmitted to the interior ; whereas in water above 45° Fahrenheit, as soon as the upper... | |
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... but the land and water are cooled by this operation in a very different manner : the impression of cooling on the land is limited to the surface, and very slowly transmitted to the interior ; whereas in water above... 
