Elementary Meteorology
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In our eReader you can find the full English version of the book. Read Elementary Meteorology Online - link to read the book on full screen. Our eReader also allows you to upload and read Pdf, Txt, ePub and fb2 books. In the Mini eReder on the page below you can quickly view all pages of the book - Read Book Elementary Meteorology
What reading level is Elementary Meteorology book?
To quickly assess the difficulty of the text, read a short excerpt:
CHAPTER IX.
DEW, FROST AND CLOUDS.
180. Condensation. The natural processes of condensation of the water vapor in the atmosphere all depend on a decrease of temperature. It is possible in the laboratory to produce condensation by the compression of moist air, the temperature in the meantime being maintained at a constant value ; but this process has practically no application in meteorology ; for when air containing vapor is compressed, as in a descending current, the diminution of capacity res...ulting from decrease of volume is more than made up by the increase of capacity resulting from increase of temperature ; and descending currents for this reason soon become dry.
Condensation as a result of cooling the air has already been briefly referred to in Section 172. Any mass of air containing vapor will, if cooled sufficiently, be reduced to the dew-point, and if the cooling then proceeds further, progres- sive condensation will accompany it. If condensation occurs at temperatures above 32°, the product will be water ; if below 32°, it will be ice in the form of frost, snow or hail.
What to read after Elementary Meteorology?
You can find similar books in the "Read Also" column, or choose other free books by Davis, William Morris, 1850-1934 to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
CHAPTER IX.
DEW, FROST AND CLOUDS.
180. Condensation. The natural processes of condensation of the water vapor in the atmosphere all depend on a decrease of temperature. It is possible in the laboratory to produce condensation by the compression of moist air, the temperature in the meantime being maintained at a constant value ; but this process has practically no application in meteorology ; for when air containing vapor is compressed, as in a descending current, the diminution of capacity res...ulting from decrease of volume is more than made up by the increase of capacity resulting from increase of temperature ; and descending currents for this reason soon become dry.
Condensation as a result of cooling the air has already been briefly referred to in Section 172. Any mass of air containing vapor will, if cooled sufficiently, be reduced to the dew-point, and if the cooling then proceeds further, progres- sive condensation will accompany it. If condensation occurs at temperatures above 32°, the product will be water ; if below 32°, it will be ice in the form of frost, snow or hail.
What to read after Elementary Meteorology?
You can find similar books in the "Read Also" column, or choose other free books by Davis, William Morris, 1850-1934 to read onlineMoreLess
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