Research Article
Effects of Geopotential and Atmospheric Drag Effects on Frozen Orbits Using Nonsingular Variables
Table 1
Frozen elements maximum variation for each dynamic model.
| Initial conditions | | | + drag | + drag | | | | (°) | | (°) | | (°) | | (°) |
| 0.001193 | 90° | 2.32E − 04 | 13.583 | 1.36E − 04 | 7.390 | 2.31E − 04 | 13.486 | 1.35E − 04 | 7.322 | 0.001193 | 100° | 3.86E − 04 | 20.195 | 3.38E − 04 | 16.548 | 3.83E − 04 | 19.964 | 3.35E − 04 | 16.360 | 0.001193 | 110° | 6.81E − 04 | 33.496 | 6.64E − 04 | 29.996 | 6.76E − 04 | 33.200 | 6.58E − 04 | 29.728 | 0.001193 | 120° | 1.02E − 03 | 50.737 | 1.02E − 03 | 46.574 | 1.01E − 03 | 50.209 | 1.01E − 03 | 46.111 | 0.001193 | 130° | 1.38E − 03 | 91.747 | 1.36E − 03 | 73.663 | 1.36E − 03 | 84.792 | 1.35E − 03 | 72.323 |
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