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|| λ degrees || acceleration || λ change || ΔV || || Longitude || × 1e-9 m/s² || 0.001°/s² || m/s/y || || 0 W || || 15 W || |
East-west acceleration, extrapolated from table 2, pp 287 || λ degrees || acceleration || λ change || ΔV per year || Δλ || || Longitude || × 1e-9 m/s² || 0.001°/day² || m/s/y || °/year² || ||<)> 0 W ||<)> 21.3 W ||<)> 0.65 W ||<)> 0.67 W ||<)> 87 W || ||<)> 15 W ||<)> 6.3 E ||<)> 0.19 E ||<)> 0.20 E ||<)> 25 W || ||<)> 30 W ||<)> 29.6 E ||<)> 0.90 E ||<)> 0.97 E ||<)> 120 E || ||<)> 45 W ||<)> 43.5 E ||<)> 1.33 E ||<)> 1.38 E ||<)> 177 E || ||<)> 60 W ||<)> 46.5 E ||<)> 1.42 E ||<)> 1.47 E ||<)> 189 E || ||<)> 75 W ||<)> 38.7 E ||<)> 1.18 E ||<)> 1.22 E ||<)> 157 E || ||<)> 90 W ||<)> 22.3 E ||<)> 0.68 E ||<)> 0.71 E ||<)> 91 E || ||<)> 105 W ||<)> 0.3 E ||<)> 0.01 E ||<)> 0.01 E ||<)> 1 E || ||<)> 120 W ||<)> 23.3 W ||<)> 0.71 W ||<)> 0.73 W ||<)> 95 W || ||<)> 135 W ||<)> 43.0 W ||<)> 1.31 W ||<)> 1.36 W ||<)> 175 W || ||<)> 150 W ||<)> 54.4 W ||<)> 1.63 W ||<)> 1.69 W ||<)> 217 W || ||<)> 165 W ||<)> 50.8 W ||<)> 1.55 W ||<)> 1.60 W ||<)> 207 W || ||<)> 180 W ||<)> 34.2 W ||<)> 1.04 W ||<)> 1.08 W ||<)> 139 W ||<)> 165 E ||<)> 6.6 W ||<)> 0.02 W ||<)> 0.21 W ||<)> 3 W || ||<)> 165 E ||<)> 6.6 W ||<)> 0.02 W ||<)> 0.21 W ||<)> 3 W || ||<)> 150 E ||<)> 25.3 E ||<)> 0.77 E ||<)> 0.80 E ||<)> 103 E || ||<)> 135 E ||<)> 52.3 E ||<)> 1.59 E ||<)> 1.65 E ||<)> 212 E || ||<)> 120 E ||<)> 65.3 E ||<)> 1.99 E ||<)> 2.06 E ||<)> 265 E || ||<)> 105 E ||<)> 58.9 E ||<)> 1.79 E ||<)> 1.86 E ||<)> 239 E || ||<)> 90 E ||<)> 34.5 E ||<)> 1.05 E ||<)> 1.09 E ||<)> 140 E || ||<)> 75 E ||<)> 0.0 W ||<)> 0.0 W ||<)> 0.0 W ||<)> 0.0 W || ||<)> 60 E ||<)> 33.0 W ||<)> 1.01 W ||<)> 1.04 W ||<)> 135 W || ||<)> 45 E ||<)> 54.3 W ||<)> 1.65 W ||<)> 1.71 W ||<)> 220 W || ||<)> 30 E ||<)> 58.3 W ||<)> 1.77 W ||<)> 1.84 W ||<)> 236 W || ||<)> 15 E ||<)> 45.5 W ||<)> 1.38 W ||<)> 1.44 W ||<)> 184 W || NOTE: large Δλ isn't "real", but implies a large oscillation and reversal. The oscillation is not sinusoidal, because the "restoring force" isn't linear with distance from "center" The above table is for east/west oscillations due to the Earth's sideways bulges, in the absence of tidal forces from the Moon and the Sun. There will also be large accelerations east/west and north/south from lunar and solar tides. As a wild guess, whatever vertical effect that tides have on the ocean will be magnified some power of the GEO radius in earth radius units (6.61) |
Soop
Handbook of Geostationary Orbits
E. M. Soop, 1983
East-west acceleration, extrapolated from table 2, pp 287
λ degrees |
acceleration |
λ change |
ΔV per year |
Δλ |
|||||
Longitude |
× 1e-9 m/s² |
0.001°/day² |
m/s/y |
°/year² |
|||||
0 W |
21.3 W |
0.65 W |
0.67 W |
87 W |
|||||
15 W |
6.3 E |
0.19 E |
0.20 E |
25 W |
|||||
30 W |
29.6 E |
0.90 E |
0.97 E |
120 E |
|||||
45 W |
43.5 E |
1.33 E |
1.38 E |
177 E |
|||||
60 W |
46.5 E |
1.42 E |
1.47 E |
189 E |
|||||
75 W |
38.7 E |
1.18 E |
1.22 E |
157 E |
|||||
90 W |
22.3 E |
0.68 E |
0.71 E |
91 E |
|||||
105 W |
0.3 E |
0.01 E |
0.01 E |
1 E |
|||||
120 W |
23.3 W |
0.71 W |
0.73 W |
95 W |
|||||
135 W |
43.0 W |
1.31 W |
1.36 W |
175 W |
|||||
150 W |
54.4 W |
1.63 W |
1.69 W |
217 W |
|||||
165 W |
50.8 W |
1.55 W |
1.60 W |
207 W |
|||||
180 W |
34.2 W |
1.04 W |
1.08 W |
139 W |
165 E |
6.6 W |
0.02 W |
0.21 W |
3 W |
165 E |
6.6 W |
0.02 W |
0.21 W |
3 W |
|||||
150 E |
25.3 E |
0.77 E |
0.80 E |
103 E |
|||||
135 E |
52.3 E |
1.59 E |
1.65 E |
212 E |
|||||
120 E |
65.3 E |
1.99 E |
2.06 E |
265 E |
|||||
105 E |
58.9 E |
1.79 E |
1.86 E |
239 E |
|||||
90 E |
34.5 E |
1.05 E |
1.09 E |
140 E |
|||||
75 E |
0.0 W |
0.0 W |
0.0 W |
0.0 W |
|||||
60 E |
33.0 W |
1.01 W |
1.04 W |
135 W |
|||||
45 E |
54.3 W |
1.65 W |
1.71 W |
220 W |
|||||
30 E |
58.3 W |
1.77 W |
1.84 W |
236 W |
|||||
15 E |
45.5 W |
1.38 W |
1.44 W |
184 W |
NOTE: large Δλ isn't "real", but implies a large oscillation and reversal. The oscillation is not sinusoidal, because the "restoring force" isn't linear with distance from "center"
The above table is for east/west oscillations due to the Earth's sideways bulges, in the absence of tidal forces from the Moon and the Sun. There will also be large accelerations east/west and north/south from lunar and solar tides. As a wild guess, whatever vertical effect that tides have on the ocean will be magnified some power of the GEO radius in earth radius units (6.61)