“…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.…”