Table 6. The magnitude of error Δh corresponding to different values of S in the equatorial plane.
From: Explicitly computing geodetic coordinates from Cartesian coordinates
S (km) | 1 | 10 | 20 | 40 | 42 | 42.6* | 43 | 45 |
Δh (m) | 103 | 102 | 101 | 102 | 104 | 10∞ | 104 | 102 |
S (km) | 60 | 80 | 200 | 400 | 800 | 1600 | 3200 | 6300 |
Δh (m) | 100 | 10−1 | 10−2 | 1010−4 | 1010−5 | 1010−6 | 1010−8 | 1010−9 |