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What's the mechanism by which the Earth pushes back on the Sun in order to conserve angular momentum for the (isolated) system as a whole??
Please show us where anyone here said that the solid Earth and its atmosphere don't exchange angular momentum?
Also these transfer happen by way of friction and friction is a non-conservative force.
So at the risk of repeating myself the Earth is not an isolated system
I already explained this to you in a previous thread.Quote from: Bored chemist on 10/09/2020 08:47:48It is, as you keep stressing the importance of the fact, an isolated system.The atmosphere can't push the world for the same reason that the man on the truck bed can't push the truck.You seem to be trying to elevate the terms isolated and closed to the status of holy writ.It's not magical.Classically:(1) A system to which you can't add or remove stuff will not change mass(2) A system to which you can't add or remove energy will change energy(3)A system to which you can not apply a force will not change momentum.(4) A system to which you can't apply a torque will not change angular momentum.Those are pretty much tautologically true.Since Einstein's day the first pair of those are a bit more flexible, but only in a very clearly defined way.Historically, in thermodynamics it was important to lump together some of those statements of the obvious.If you have a system to which you can add or subtract matter then you can't sensibly define what it will do- because it depends on the matter you might add.The same goes for applying forces to it. Those forces just complicate the issue.So, they invented the "closed system" where tautologies 1 and 3 apply. Similarly, for some calculations, you want to prevent energy entering or leaving the system.And that's why they invented the "isolated system"- as a shorthand for a system where tautology 2 also applies.If thermodynamics dealt with angular momentum they would have invented another term for systems where tautology 4 also applied. They didn't.But, if they had done, the Earth would be on the list.
I have been stating on numerous posts, that the transfers between the solid surface and the atmosphere are partially inelastic, So the exchange of angular momentum will not be able to return the same value of momentum back to the rotating solid earth, to maintain the LOD.
then it requires explanations of phenomena such as the transfer of momentum via sound waves t
Quote from: gem on 03/09/2021 11:12:17 then it requires explanations of phenomena such as the transfer of momentum via sound waves tThe explanation isn't very complex.Molecule A hits molecule B.Momentum and energy are conserved in this process.So they are also conserved in any process which is a succession of repetitions of that step.
Ok so the collision occurs transferring momentum away from direction of the angular velocity
Given the Inverse square law of sound waves
Also given the time aspect between transfers how do you exclude thermal radiation in your calculations spontaneously transfering away from that side of the equation
You are muddling a whole bunch of things there.Please clarify your question in terms of angular momentum;linear momentum and energy, all of which are strictly conserved
Are you aware that sound does not follow the inverse square law?
The sound intensity from a point source of sound will obey the inverse square law
Also given the time aspect between transfers how do you exclude thermal radiation in your calculations spontaneously transferring away from that side of the equation
I don't need to. All transfers, including those carried by photons, conserve momenta and energy
Sorry BC, I don't agree,
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
indeed as you say photons conserve momenta and energy but the system does not.
"Stokes's law of sound attenuation is a formula for the attenuation of sound in a Newtonian fluid, such as water or air, due to the fluid's viscosity. It states that the amplitude of a plane wave decreases exponentially with distance travelled,"
For the elasticity of the collisions to be immaterial, then it requires explanations of phenomena such as the transfer of momentum via sound waves the majority that also end up as heat, retrieved to the angular momentum.
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 ?
It is zero.As you say, it points equally in all directions and the only way to do that is to have all the vectors "cancel out".
Therefore, calculation of the total change in intensity involves the inverse-square law and an estimation of attenuation over the path due to the viscosity of the medium.
precisely the solid earth transferred angular momentum to the atmosphere reducing the solid earths momentum total.
Quote from: gem on 06/09/2021 23:35:47precisely the solid earth transferred angular momentum to the atmosphere reducing the solid earths momentum total.Which as you say the momentum carried away by sound to be available to be transferred back later is ZERO The solid earth (over a reasonable period of time) transfers ZERO momentum to the atmosphere.Because the momentum carried by the sound sums to zero.So the loss by the solid earth is zero.If the Earth lost angular momentum to the air then the air would have to rotate WRT the earth.Friction would slow it down again until the angular momentum was transferred back.In the short term, there can be transfers (though they are very near zero on average across the Earth).Averaged over time they are exactly zero. |(Give or take atmospheric tidal drag).
precisely the solid earth transferred angular momentum to the atmosphere reducing the solid earths momentum total.Which as you say the momentum carried away by sound to be available to be transferred back later is ZERO
If we consider the approximate 0.3 of a milli second variation for one day given in the dates earlier, corresponds to a change in rotational kinetic energy of the solid earth in the region of 1.6 x 10^21 joules for the day in question.
The annual component of the change of the length of day of approx 0.34 ms...If we consider the approximate 0.3 of a milli second variation for one day
Quote from: gem on 08/09/2021 00:11:02If we consider the approximate 0.3 of a milli second variation for one day given in the dates earlier, corresponds to a change in rotational kinetic energy of the solid earth in the region of 1.6 x 10^21 joules for the day in question.I realise it's terribly "English" to always talk about the weather but...We are talking about the momentum transfers which definitely sum to zero over the long term.You are talking about the transfer of heat from the earth to the air.And that's broadly what drives the weather.So it is irrelevant.The hint is in the units.
I don't know where the variation of 0.3ms in one day came from. This quotes an annual change, not a 1 day change.