“…+β 3 cos (4i) + β 4 cos (6i)) + J 3 2 R 6 n t a 6 (︀ 1 − e 2 )︀ 19/2 (β5 where the subscript (ob) stands for oblateness, µ is the Newtonian constant times mass of Earth, R the mean equatorial radius of the Earth, ω the argument of the perigee, J k the zonal harmonics, given by J 2 = 1.08263 × 10 −3 , J 3 = − 2.5322 × 10 −6 , J 4 = −1.6110 × 10 −6 , D 4 = J 2 2 + J 4 = −0.4389122 × 10 −6 , and α i and β j , i = 1, . .…”