1974
DOI: 10.1007/bf01260515
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Lunar perturbations of artificial satellites of the earth

Abstract: Abstract. Lunisolar perturbations of an artificial satellite for general terms of the disturbing function were derived by Kaula (1962). However, his formulas use equatorial elements for the Moon and do not give a definite algorithm for computational procedures. As Kozai (1966Kozai ( , 1973 noted, both inclination and node of the Moon's orbit with respect to the equator of the Earth are not simple functions of time, while the same elements with respect to the ecliptic are well approximated by a constant and a l… Show more

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Cited by 50 publications
(44 citation statements)
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“…Since algebraic errors appear in the mathematics leading to equation (15) in [2], equations (15 to 19) there are false; but the form of (19) is desirable, and so the mathematics which follow will be aimed toward the objective of producing a similar form. Suppose m is even and / -777 is even, then Employing the identity cos(x -f) = sinx.…”
Section: Ft = Izmentioning
confidence: 99%
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“…Since algebraic errors appear in the mathematics leading to equation (15) in [2], equations (15 to 19) there are false; but the form of (19) is desirable, and so the mathematics which follow will be aimed toward the objective of producing a similar form. Suppose m is even and / -777 is even, then Employing the identity cos(x -f) = sinx.…”
Section: Ft = Izmentioning
confidence: 99%
“…Now Giacaglia proceeded to average (2.6) over the mean anomaly of the satellite to produce the secular and long periodic parts of the disturbing function together with the short period corrections, and a solution is certainly possible by this route, but since the real advantage of (2.6) lies in the fact that it paves the way for simultaneous integration of the angular rates for the satellite and the Moon, we will defer averaging techniques to the next section where all averaging is performed on the outset directly from (1.2). Therefore, we will skip to (117) in [2], where the true anomalies of the satellite and the Moon are converted to their respective mean anomalies via the Hansen coefficients, which satisfy the equation If the mean motion n is approximated as n = no(l - §^f )> where 6a is the perturbation of the semimajor axis due to a above, and R^ is substituted for R in the Lagrange equations, then a complete integration of the system is possible provided a,a^,e,e^., I, Ik, i, -A/, 3/fc,w, Wfc, fi, Qk are ah held fixed and constant throughout the integration. Numerical tests show that this approximation is improved over the long term if the mean values for these constants are used instead of the initial value conditions.…”
Section: Ft = Izmentioning
confidence: 99%
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“…It is the intent for the numerical examples to highlight the simplifying issues mentioned above. The first method to be presented will be called the 'series expansion method' and follows the development of Kaula [5] and Giacaglia [2]. We will refer to this solution as the (SEM) solution.…”
Section: Introductionmentioning
confidence: 99%