 | Monthly literary register - 1820 - 694 páginas
...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 páginas
...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...supplied by warmer water from below. The surface of the water will, therefore, in calm and clear weather, and temperatures above 45° Fahrenheit, be warmer... | |
 | 1820 - 442 páginas
...greatest deviation when the ship's head is N. or S. METEOROLOGY. 12. Sir H. Davy's Theory of Mists. — According to this eminent chemist, land and water...supplied by warmer water from below. The surface of the water will therefore, in calm and clear weather, and in temperatures above 45* Fahr., be warmer... | |
 | 1820 - 468 páginas
...ship's head is N. or S. METEOROLOGY. 12. Sir H. Davy's Theory of Mists. — According to this emi, nent chemist, land and water are cooled after sunset in...supplied by warmer water from below, The surface of the water will therefore, in calm and clear weather, and in temperatures above 45* Fahr., be warmer... | |
 | 1821 - 488 páginas
...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 páginas
...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 páginas
...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 páginas
...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... | |
 | Sir Richard Phillips - 1830 - 728 páginas
...deviation when the ship's head is north or south. Theory of Mists. By Sir H. DJIV Y. — [ 1819. ] LAND and water are cooled after sunset in a very different...supplied by warmer water from below. The surface of the water will, therefore, in calm and clear weather, and in temperatures above 45° Fahr., be warmer... | |
 | John Ayrton Paris - 1831 - 582 páginas
...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... | |
| |
... 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... 
