Mathematical Tracts on the Lunar and Planetary Theories, the Figure of the Earth, Precession and Nutation, the Calculus of Variations, and the Undulatory Theory of Optics: Designed for the Use of Students in the UniversityMacmillan and Company, 1858 - 400 sider |
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Side 10
... velocity , that it would have performed a revolution in the same time in which it does perform it . It is therefore called the mean anomaly . 17. If we expand these coefficients as far as e3 , or if we adopt the method of expansion in ...
... velocity , that it would have performed a revolution in the same time in which it does perform it . It is therefore called the mean anomaly . 17. If we expand these coefficients as far as e3 , or if we adopt the method of expansion in ...
Side 26
... is meant , the mean angular motion , or the velocity with which the mean longitude increases . The mean motion varies therefore inversely as the periodic time . METHOD OF ESTIMATING THE ORDERS OF TERMS . 27 small 26 . LUNAR THEORY .
... is meant , the mean angular motion , or the velocity with which the mean longitude increases . The mean motion varies therefore inversely as the periodic time . METHOD OF ESTIMATING THE ORDERS OF TERMS . 27 small 26 . LUNAR THEORY .
Side 48
... velocity which is to the whole angular velocity of M as 1 - c : 1 ; or which is to the angular velocity of M in that moveable orbit as 1 - c to c . The perigee of the Moon's orbit therefore is not fixed , but ( while we neglect the ...
... velocity which is to the whole angular velocity of M as 1 - c : 1 ; or which is to the angular velocity of M in that moveable orbit as 1 - c to c . The perigee of the Moon's orbit therefore is not fixed , but ( while we neglect the ...
Side 49
... velocity = ( 1 − c ) × whole angular velocity of the Moon . 62. For the explanation of the next term , m2 cos { ( 2 — 2m ) 0 — 2ß } , -- - we observe that { ( 1 - m ) 0 - ẞ } ( Article 48 ) is nearly the dif ference of longitude of the ...
... velocity = ( 1 − c ) × whole angular velocity of the Moon . 62. For the explanation of the next term , m2 cos { ( 2 — 2m ) 0 — 2ß } , -- - we observe that { ( 1 - m ) 0 - ẞ } ( Article 48 ) is nearly the dif ference of longitude of the ...
Side 83
... long time ) , the velocity of the planet may be increased so that it describes a larger orbit than before , and its periodic time will therefore be increased , and : that by a quantity proportional to the time of action 6-2.
... long time ) , the velocity of the planet may be increased so that it describes a larger orbit than before , and its periodic time will therefore be increased , and : that by a quantity proportional to the time of action 6-2.
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Mathematical Tracts on the Lunar and Planetary Theories, the Figure of the ... George Biddell Airy Uten tilgangsbegrensning - 1858 |
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Mathematical Tracts on the Lunar and Planetary Theories: The Figure of the ... George Biddell Airy, Sir Ingen forhåndsvisning tilgjengelig - 2016 |
Vanlige uttrykk og setninger
2π λ analyzing plate angle angular velocity attraction axes axis bright Cambridge cloth co-ordinates coefficient College Consequently constant cos² Crown 8vo crystal curve depending different colours differential direction displacement distance disturbing force dR dR dt dt Earth elliptically polarized ellipticity equal equation expression extraordinary ray Fcap front ƒ² glass Hence inclined integration intensity investigation length longitude mean anomaly Moon motion multiplied nearly node nutation ordinary ray parallel particles perigee perihelion perpendicular plane of incidence plane of polarization plane of reflection precession principal plane produced PROP proportion quantity radius vector refraction rhombohedron rings shew sin² spheroid Sun's suppose surface tion tourmaline Trinity College undulation vibration vt-x wave
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