Mathematical And Physical Papers
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In our eReader you can find the full English version of the book. Read Mathematical And Physical Papers 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 Mathematical And Physical Papers
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Dr Young's formula is based on the principle of taking into account the attraction of the table-land existing between the station and the level of the sea, in reducing the observation to the sea level. On account of this attraction, the multiplier 2/i/a which gives the correction for elevation alone must be reduced in the ratio of 1 to l-Scrjip, or 1 to '66 nearly, if (t = 2J, /) = 5.V. Mr Airy, observing that the value cr = 2J is a Uttlc too small, and p = 5i a little too great, has emijloycd ...the factor -C, instead of -66.
AT THE SURFACE OF THE EARTH. 151 17. Consider first the value of G. We have by the preceding formula, and the first of equations (27), G = xa [g,) + Gk -00017 m Qi).
According to Professor Eigaud's determination, the quantity of land on the surface of the earth is to that of water as 100 to 276*.
If we suppose the mean elevation of the land ith of a mile, and the mean depth of the sea 3^ miles, we shall have ., f x3-|x276 --ixl00 m («) = - gyg ° = - 1-49 nearly ; so that the value of G determined by g^ would be too great by about ■000253 of the whole.
What to read after Mathematical And Physical Papers?
You can find similar books in the "Read Also" column, or choose other free books by Rayleigh, John William Strutt, Baron, 1842-1919 to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
Dr Young's formula is based on the principle of taking into account the attraction of the table-land existing between the station and the level of the sea, in reducing the observation to the sea level. On account of this attraction, the multiplier 2/i/a which gives the correction for elevation alone must be reduced in the ratio of 1 to l-Scrjip, or 1 to '66 nearly, if (t = 2J, /) = 5.V. Mr Airy, observing that the value cr = 2J is a Uttlc too small, and p = 5i a little too great, has emijloycd ...the factor -C, instead of -66.
AT THE SURFACE OF THE EARTH. 151 17. Consider first the value of G. We have by the preceding formula, and the first of equations (27), G = xa [g,) + Gk -00017 m Qi).
According to Professor Eigaud's determination, the quantity of land on the surface of the earth is to that of water as 100 to 276*.
If we suppose the mean elevation of the land ith of a mile, and the mean depth of the sea 3^ miles, we shall have ., f x3-|x276 --ixl00 m («) = - gyg ° = - 1-49 nearly ; so that the value of G determined by g^ would be too great by about ■000253 of the whole.
What to read after Mathematical And Physical Papers?
You can find similar books in the "Read Also" column, or choose other free books by Rayleigh, John William Strutt, Baron, 1842-1919 to read onlineMoreLess
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