Journal of the Transactions of the Victoria Institute, Or Philosophical Society of Great Britain, Том 13Victoria Institute., 1880 |
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Стр. 21
... mean rainfall of our island is 32 inches . Without some unproved change in the physical conditions , the rainfall of the winter months would be less than 20 inches , or if snow be reckoned six times lighter than water , this would ...
... mean rainfall of our island is 32 inches . Without some unproved change in the physical conditions , the rainfall of the winter months would be less than 20 inches , or if snow be reckoned six times lighter than water , this would ...
Стр. 22
... means of lessening the difference of sensible heat in different seasons of the year . When the radiation is in excess of the supply of solar heat , the freezing of water sets free 140 ° of heat to repair the loss ; and when the summer ...
... means of lessening the difference of sensible heat in different seasons of the year . When the radiation is in excess of the supply of solar heat , the freezing of water sets free 140 ° of heat to repair the loss ; and when the summer ...
Стр. 23
... area or basin , from 25 ° N. up to the Arctic Circle . The consequent increase of the mean tempera- ture of Great Britain is not less , he thinks , than 30 ° ; but in estimating the temperature for his glacial epoch this element is 23.
... area or basin , from 25 ° N. up to the Arctic Circle . The consequent increase of the mean tempera- ture of Great Britain is not less , he thinks , than 30 ° ; but in estimating the temperature for his glacial epoch this element is 23.
Стр. 24
... mean temperature of space , or - 239 ° F. , being determined by a simple rule - of - three calculation . And since the winter northern solstice is now very near the perihelion , the present excess above the average value , when combined ...
... mean temperature of space , or - 239 ° F. , being determined by a simple rule - of - three calculation . And since the winter northern solstice is now very near the perihelion , the present excess above the average value , when combined ...
Стр. 26
logarithms of radius vector , change of midwinter heat com- pared with a mean distance , and results for Great Britain . 88 • 0415 302 ° 47 ' ⚫01564 16 ° .18 48 ° • 41 87 * 0544 135 ° 7 ′ ! -'01572 - 17 ° 07 15 ° .16 86 • 0631 326 ° 0 ...
logarithms of radius vector , change of midwinter heat com- pared with a mean distance , and results for Great Britain . 88 • 0415 302 ° 47 ' ⚫01564 16 ° .18 48 ° • 41 87 * 0544 135 ° 7 ′ ! -'01572 - 17 ° 07 15 ° .16 86 • 0631 326 ° 0 ...
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