Practical Meteorology
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In our eReader you can find the full English version of the book. Read Practical 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 Practical Meteorology
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To quickly assess the difficulty of the text, read a short excerpt:
By using melting ice for the freezing- 130 PRACTICAL METEOROLOGY.
point, and freezing mixtures for temperatures still lower, this table has been carried to a great extent ; above the boiling-point hot. Oil has been made use of; but for the purposes of meteorology, the table of the tension or elasticity of aqueous vapour may be confined to much narrower limits.
If the space above the liquid in the barometric tube is occupied by air (or indeed by any perma- nent gas), the vapour of water will fol...low the same laws as regulate it in vacuo, that is, the same relation will be preserved between the density, tension, and temperature ; they will, in fact, be precisely the same as in vacuo, with this difference only, that, while in vacuo the quantity of vapour necessary to saturate the space above the column is formed instantaneously, time is re- quisite for the evaporation to go on in air.
The conclusions of Dalton have been confirmed more recently by Dr. Ure, Regnault, and others ; they have been the foundation of tables showing the elastic force of vapour, as measured in inches of mercury, for all degrees of temperature.
What to read after Practical Meteorology?
You can find similar books in the "Read Also" column, or choose other free books by John Drew to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
By using melting ice for the freezing- 130 PRACTICAL METEOROLOGY.
point, and freezing mixtures for temperatures still lower, this table has been carried to a great extent ; above the boiling-point hot. Oil has been made use of; but for the purposes of meteorology, the table of the tension or elasticity of aqueous vapour may be confined to much narrower limits.
If the space above the liquid in the barometric tube is occupied by air (or indeed by any perma- nent gas), the vapour of water will fol...low the same laws as regulate it in vacuo, that is, the same relation will be preserved between the density, tension, and temperature ; they will, in fact, be precisely the same as in vacuo, with this difference only, that, while in vacuo the quantity of vapour necessary to saturate the space above the column is formed instantaneously, time is re- quisite for the evaporation to go on in air.
The conclusions of Dalton have been confirmed more recently by Dr. Ure, Regnault, and others ; they have been the foundation of tables showing the elastic force of vapour, as measured in inches of mercury, for all degrees of temperature.
What to read after Practical Meteorology?
You can find similar books in the "Read Also" column, or choose other free books by John Drew to read onlineMoreLess
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