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believe we already covered the universal link (momentum = energy/phase velocity.)
In every single collision between any two atoms or between atoms and photons or phonons, momenta and energy are conserved.So they must be conserved in every sequence and combination of collisions.
I pointed out that sound waves spread in all directions, so their vector sum is zero.That cover it nicely.
The problem with that is,the momentum and energy of sound is carried off in all directions.which brings us back to, how is the vector direction total maintained for later transfer back to the angular momentum of the solid earth, due to the partially inelastic collisions sending momentum away from the transfer point, in all directions ?
How does the addition work for a non isolated system ?
So the problem still remains, a daily change in angular momentum vector due to friction ending up as momentum with a positive value but no longer having a net direction to transfer back to maintain/conserve the LOD
I realise it's terribly "English" to always talk about the weather but...
1.6 x 10^21 joules for the day
If the loss is (on average) isotropic then the net change in momentum is (on average) zero
The earliest observations of changes in length of day were made at Paris Observatory by Stoykoand Stoyko (1936), who observed the annual variation of length of day. In 1948, Victor Starr of theMassachusetts Institute of Technology (MIT) noted that the atmosphere need not conserve angularmomentum, and could share it with the Earth below. Starr started the General Circulation Projectat MIT, and one of its features was calculations of fluxes and changes in atmospheric angularmomentum.
As Paul Simon said, "the problem is all inside your head""The answer is easy , if you take it logically."This "a daily change in angular momentum vector due to friction "Just isn't real.
The problem with that statement is the frictional coupling between the solid earth and its atmosphere converts anisotropic motion to isotropic motion.
You also seem not to recognise that, on any given day, the angular momentum of the atmosphere may be a bit higher or lower than the average
It is conserved because there is no torque acting on the system (apart from a few thing we have discussed, such as the tides).
I believe it can be explained as terminal velocity.
To explain these forces although a simple mechanism, I will have to go across a broad range of examples and correlations of physical events.