The Quarterly Journal, Том 20John Murray, 1826 |
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Страница 12
... quantity of vapour contained in the air . The elevation of those mists above the surface of the sea will also be regulated by that of the icebergs , near which they form ; since the cooling influence of the frozen mass , by rapidly dimi ...
... quantity of vapour contained in the air . The elevation of those mists above the surface of the sea will also be regulated by that of the icebergs , near which they form ; since the cooling influence of the frozen mass , by rapidly dimi ...
Страница 15
... quantity of moisture occasioned an error of such magnitude , that , of gases which are now known to expand alike , some appeared to dilate five times as much as others by the same application of heat . * Journal de l'Ecole Polytechnique ...
... quantity of moisture occasioned an error of such magnitude , that , of gases which are now known to expand alike , some appeared to dilate five times as much as others by the same application of heat . * Journal de l'Ecole Polytechnique ...
Страница 16
... quantity of water which must at some periods pass , in a very short space of time , from the state of transparent vapour to that of clouds or rain . If we fully consider the extent and magnitude of these pheno- mena , we must conceive ...
... quantity of water which must at some periods pass , in a very short space of time , from the state of transparent vapour to that of clouds or rain . If we fully consider the extent and magnitude of these pheno- mena , we must conceive ...
Страница 18
... quantity § . " Mr. Dalton ob serves , " the barometer generally rises with a wind between the north and east , and is very low in winter when a strong and warm S. or S.W. wind blows ] . " He adds , the lowest extreme of the barometer ...
... quantity § . " Mr. Dalton ob serves , " the barometer generally rises with a wind between the north and east , and is very low in winter when a strong and warm S. or S.W. wind blows ] . " He adds , the lowest extreme of the barometer ...
Страница 20
... quantity of water in the atmosphere is not sufficient to account for the move- ments of the barometer , and for winds , from the changes in its state from transparent vapour to that of clouds or rain . To this objection I would reply ...
... quantity of water in the atmosphere is not sufficient to account for the move- ments of the barometer , and for winds , from the changes in its state from transparent vapour to that of clouds or rain . To this objection I would reply ...
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