Table 8. The magnitude of error Δh corresponding to different values of S in the region except near the center, the polar axis and the equatorial plane.
From: Explicitly computing geodetic coordinates from Cartesian coordinates
S (km) | 31 | 34 | 78 | 178 | 378 | 1000 | 3000 | 6300 |
Δh (m) | 103 | 102 | 10−1 | 10−2 | −4 | −6 | 10−8 | 10−9 |