- #71
Andre
- 4,311
- 74
It is building very gradually just a bit in analogy like this:
http://www.astronomynotes.com/gravappl/s10.htm
The differential gravity pull of Earth and Moon as in the third figure shows an example of exchange of momentum. Similar to the process of the moon, the assymetric gravity on the previous equatorial bulge of Venus pulls the planet ahead of its orbit, resulting in a slow spiral outwards. As the radius of the orbit increases the angular momentum of its spin transfers to the orbit of the planet.
Parameters are quite different of course and the process with Venus was likely more complicated. A tidal bulge is much smaller than a planets equatorial bulge.
I propose the next process:
In case of precession, the angular momentum vector is changing direction. Looking at the vector compounds in two dimensions, transfer of momentum takes place in both dimension and back when a precession cycle is completed. The sun in the Earth precession cycle gravity interactions "takes"a proportional part of the momentum in the first stage of the precession cycle in one dimension and "gives it back" in the final stage, transferring it between the two dimensions. However it is possible that a part of the momentum vector, that of the core, is getting misaligned. Then this process of transferring momentum between the dimensions is only taking place on the mantle part of the angular momentum. With diverging vectors the numerical vector is always less than that of the components. When the core and mantle realign in a chaotic process, dissipating a lot of energy, then the momentum at that moment is fixed at a lesser value and when the gravity interaction "gives" momentum back, it is still proportional, to the lesser value. So not all spinning momentum is retransferred. An this went on for millions perhaps billions of years repeating the process about every 100,000 years.
http://www.astronomynotes.com/gravappl/s10.htm
The differential gravity pull of Earth and Moon as in the third figure shows an example of exchange of momentum. Similar to the process of the moon, the assymetric gravity on the previous equatorial bulge of Venus pulls the planet ahead of its orbit, resulting in a slow spiral outwards. As the radius of the orbit increases the angular momentum of its spin transfers to the orbit of the planet.
Parameters are quite different of course and the process with Venus was likely more complicated. A tidal bulge is much smaller than a planets equatorial bulge.
I propose the next process:
In case of precession, the angular momentum vector is changing direction. Looking at the vector compounds in two dimensions, transfer of momentum takes place in both dimension and back when a precession cycle is completed. The sun in the Earth precession cycle gravity interactions "takes"a proportional part of the momentum in the first stage of the precession cycle in one dimension and "gives it back" in the final stage, transferring it between the two dimensions. However it is possible that a part of the momentum vector, that of the core, is getting misaligned. Then this process of transferring momentum between the dimensions is only taking place on the mantle part of the angular momentum. With diverging vectors the numerical vector is always less than that of the components. When the core and mantle realign in a chaotic process, dissipating a lot of energy, then the momentum at that moment is fixed at a lesser value and when the gravity interaction "gives" momentum back, it is still proportional, to the lesser value. So not all spinning momentum is retransferred. An this went on for millions perhaps billions of years repeating the process about every 100,000 years.
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