 ... believed that that increase will be more than counterbalanced by the 140° of heat given out, in the case of hail, at the moment of congelation, for which no allowance is made in the above calculation. It follows, then, from the principle here demonstrated,...  The American Meteorological Journal - Page 41888Full view - About this book
 | 1836 - 950 pages
...follows, then, from the principle here demonstrated, that the moment a portion of transparent vapour in the air begins to condense into cloud, the air...temperature is greater than that of the surrounding air. Without examining its condition every instant of its ascent, let us imagine it to have ascended three... | |
 | 1836 - 1042 pages
...follows, then, from the principle here demonstrated, that the moment a portion of transparent vapour in the air begins to condense into cloud, the air...temperature is greater than that of the surrounding air. Without examining its condition every instant of its ascent, let us imagine it to have ascended three... | |
 | 1837 - 524 pages
...a portion of the transparent vapor in the air begins to condense into ci ua, me air in which it is begins to expand, and, consequently, if an equilibrium...temperature is greater than that of the surrounding air." We omit some remarks, and calculations, elucidating the change of the dew-point, and of the temperature... | |
 | Elias Loomis - 1868 - 328 pages
...production of a cloud, the air in the cloud is warmed; it expands in volume, and the cloud continues to ascend as long as its temperature is greater than that of the surrounding air. As the cloud ascends, more vapor is condensed, while the latent heat evolved raises still farther the... | |
 | 1836 - 494 pages
...follows, then, from the principle here demonstrated, that the moment a portion of transparent vapour in the air begins to condense into cloud, the air...temperature is greater than that of the surrounding air. Without examining its condition every instant of its ascent, let us imagine it to have ascended three... | |
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