^ At least one of us is misunderstanding the mechanics involved in tidal locking.
As I understand it, in the familiar Earth-Moon case (considering the Moon only as a source of tidal forces and Earth only as their subject, since the Moon is of course already locked), the Moon creates tides on Earth, and the effect of these tides is to gradually dissipate Earth's rotational energy. Part of it goes into accelerating the Moon, which puts it into a higher orbit, part of it is spend as friction heat et cetera. This will continue until Earth is tidally locked (the tidal bulges have to move relative to surface and/or have varying amplitudes to be able to dissipate energy). Or, rather, it
would continue until then, if the timescale didn't exceed the remaining lifetime of the solar system in its present form.
So, yes, you were speaking of tidally locking the Sun when you were speaking of increasing the planets' angular momentum, since those two effects are two sides of the same coin and cannot be separated. If you have a timescale for the one, you have a timescale for the other.
H2Bro said:
[...] insert figure skater reference here [...]
A figure skater is a solid body, meaning all parts of one have to spin with the same angular speed. If they enlarge the "orbit" of their hands, thus lowering the hands' angular speed below their torso's, the physical link between the two parts (the arms) will transmit torques in both directions, with the result of speeding up the hands and slowing down the torso until the angular speeds are the same once more.
A solar system is gravitationally bound, meaning different parts of one have to spin/orbit with different angular speeds. If something were to enlarge the orbits of its planets, thus lowernig the planets' angular speed per Kepler's laws, there are no arms to transmit a torque to the Sun, so its angular speed wouldn't be affected.
If said something is part of the solar system, then its total angular momentum has to be conserved, just as it is for the figure skater. Other than that, though, the two cases have little in common.
H2Bro said:
Meaning a planetary body that has viscous surface which is attracted by the sun and exhibits tides - in the normal sense - will slowly drift further out as gravitational energy is consumed moving the viscous liquid against the planet's surface friction.
Tidal forces exerted by the Sun upon a planet (which isn't in tidal lock or resonance yet) dissipate the planet's rotational energy without changing the planet's orbit, as far as I know. There is simply no mechanism to do this. I suppose that if the planet in question is Jupiter, one could consider the Sun's orbit about their common centre of mass in this regard. If the tidal bulge on Jupiter leads or lags, that orbital distance could be affected, and the planet's orbital distance would have to change in turn to compensate. I'm having a bit of trouble fathoming this particular situation, to be honest. Maybe someone else can explain.
Now, tidal forces exerted by a planet upon the Sun (which definitely isn't in tidal lock or resonance yet) dissipate the Sun's rotational energy, and part of that energy can indeed be transferred to the planet's orbit.
That's what I gave you an order-of-magnitude estimate for in the previous post.
H2Bro said:
This effect is observed with the moon, which is slowly drifting further from the Earth as it pulls the oceans along whoses movements are resisted by the continents).
It is, but you have to think the analogy through very carefully to draw conclusions about the Sun-planet case: Which body takes the place of which?