 The declination of the sun, given in the Ephemeris of the Nautical Almanac, from year to year, is calculated for apparent noon at Greenwich, England. To determine it for any other hour at a place in the...  Elements of Surveying and Leveling - Página 7de Charles Davies - 1883 - 564 páginasVisualização completa - Sobre este livro
 | Gurley, W. & L. E., Troy, N.Y. - 1871 - 228 páginas
...meridional refraction for the given day, and the latitude of the place where the observation is made. To SET OFF THE DECLINATION. — The declination of...situated on, or very nearly on, the same meridian. Beyond the parallel of Santa Fe, the allowance would be about seven hours, and in California, Oregon,... | |
 | Gurley, W. & L. E., Troy, N.Y. - 1871 - 218 páginas
...meridional refraction for the given day, and the latitude of the place where the observation is made. To SET OFF THE DECLINATION. — The declination of...not given directly in the tables of the Almanac, can lie ascertained very nearly by reference to that of other places given, which are situated on, or very... | |
 | Gurley, W. & L. E., Troy, N.Y. - 1878 - 284 páginas
...hour at a place in the US, reference must be had, not only to the difference of time arising from th« longitude, but also to the change of declination from...place, and therefore its difference in time, if not givt-'i directly in the tables of t'ie Almanac, can be ascertained v<.ry nearly by reference to that... | |
 | Charles Fitzroy Bellows, Francis Hodgman - 1886 - 490 páginas
...apparent noon at Greenwich, England. To determine it for any other hour at a place in the United States, reference must be had, not only to the difference...longitude of the place, and therefore its difference mtime, if not given directly in the tables of the Almanac, can be ascertained very nearly by reference... | |
 | Daniel Carhart - 1888 - 530 páginas
...Greenwich, England, or Washington, DC To determine it for any other hour at a place in the United States, reference must be had, not only to the difference...also to the change of declination from day to day. By the use of standard time, which is now quite general throughout the United States, it is very easy... | |
 | Bennett Hooper Brough - 1888 - 366 páginas
...apparent noon at Greenwich. To determime it for any other hour at any other place, reference must be made not only to the difference of time arising from the...also to the change of declination from day to day. Thus, supposing that the observations are being made at a place eight hours west of Greenwich, the... | |
 | International Correspondence Schools - 1900 - 728 páginas
...time arising from the difference of longitude, but also to the change of declination during that time. The longitude of the place, and therefore its difference...tables of the almanac, can be ascertained very nearly hy reference to that of other places given which are situated on, or very nearly on, the same meridian.... | |
 | James Underhill - 1922 - 268 páginas
...time arising from the difference of longitude, but also to the change of declination during that time. The longitude of the place, and therefore its difference in time, if not given directly in the ephemeris, can be ascertained very nearly by reference to that of other places given which are situated... | |
 | James Underhill - 1922 - 272 páginas
...apparent noon at Greenwich, England. To determine it for any other hour at a place in the United States, reference must be had, not only to the difference of time arising from the difference of longitude, but also to the change of declination during that time. The longitude 'of... | |
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