... depression produced by radiation from some bodies may never reach it. In this case no dew could be formed upon them. It is therefore evident, that for the dewing process to begin early, and continue copiously, a very small lowering only of the heat... An Outline of the Sciences of Heat and Electricity - Page 141by Thomas Thomson - 1840 - 585 pagesFull view - About this book
| 1831 - 340 pages
...copiously, a very small lowering only of the heat of the atmospheric particles should be necessary. The temperature of the atmosphere usually sinks considerably...after sunset, and is often 20° or 30° colder than during the day. Hence, in such cases, it must approach much nearer the point of depositing moisture,... | |
| 1832 - 334 pages
...copiously, a very small lowering only of the heat of the atmospheric particles should be necessary. The temperature of the atmosphere usually sinks considerably...after sunset, and is often 20° or 30° colder than during the day. Hence, in such cases, it must approach much nearer the point of depositing moisture,... | |
| 1831 - 346 pages
...copiously, a very small lowering only of the heat of the atmospheric particles should be necessary. The temperature of the atmosphere usually sinks considerably...after sunset, and is often 20° or 30° colder than during the day. Hence, in such cases, it must approach much nearer the point of depositing moisture,... | |
| Gray and Bowen - 1831 - 348 pages
...copiously, a very small lowering only of the heat of the atmospheric particles should be necessary. The temperature of the atmosphere usually sinks considerably...after sunset, and is often 20° or 30° colder than during the day. Hence, in such cases, it must approach much nearer the point of depositing moisture,... | |
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