 | 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 - 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... | |
 | 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... | |
 | 1820 - 486 pages
...METEOBOLOC-Y. "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,...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
...and we only notice the subject, to direct attention to Sir Humphrey Davy's elegant and simple theory. According to this eminent chemist, land and water...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... 
