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On the possible reversal of an earth-scale top

Hara K.

Journal of Technical Physics

2009

Vol. 50, no 4

375-385

We work with a theory based on a hypothetical torque corresponding to the revolution gyroscope-effect, an effect ultimately caused by axial precession Φ. Applying this theory to an Earth-scale top, the reversal time from θ ≅ 180° to θ ≅ 0° can be estimated to be roughly 6 x 109 years. The reversal time from θ ≅ 180° to θ = 23.45° , meanwhile, can be estimated to be 4.6 x 109 years. This hypothetical torque can be validated by satellite experiments.