pmb_phy said:
Geodesic deviation is also not frame dependant. If it were then the Riemann tensor would also be frame dependant. A geodesic is a geometric object whose nature does't change. Tidal forces exist if and only if a spherical object placed in the field which is subject to no external sources will become deformed do to the non-vanishing Riemann tensor. The fact that the coordinate acceleeration varies with height does not mean that there is geodesic deviation. In fact if you were to calculate the deviation you'd find it to be zero.
Pete
True, but consider the Milne metric from
https://www.physicsforums.com/showpost.php?p=754243&postcount=78
<br />
ds^2 = -dt^2 + t^2 d \chi^2 + t^2 sinh(\chi)^2 d \theta^2 + t^2 sinh(\chi)^2 sin(\theta)^2 d \phi^2<br />
It has a zero Riemann.
\chi=\theta=\phi = constant are geodesics - this can be seen from the fact that the above metric is an example of a FRW metric.
Becauses the scale factor is a(t)^2 = t^2, we have the scale factor a(t)=t and thus nearby geodesics do not accelerate away from each other. Thus there is no geodesic deviation, as one would expect from a metric whose Riemann is zero and the geodesic deviation equation.
However, while the geodesics do not accelerate away from each other, they do not maintain a constant distance either. Because the geodesics are given by \chi= constant, the distance between them increases proportionally to the scale factor a(t), i.e. the distance between geodesics is proportional to time and not constant.
The distance measure used with the Milne metric is different from the distance measure used with the flat Minkowski metric, even though there is a variable transformation that maps one into the other.
i.e. if you substitute
t1 = t*cosh(\chi), r1 = -t*sinh(\chi)
into the Minkowski metric
-dt1^2 + dr1^2 + r1^2(d \theta^2 + sin(\theta)^2 d \phi^2)
you get the Milne metric.
This is an example of how distance measures are coordinate dependent - different notions of simultaneity give rise to different notions of distance.
[add]
I should probably add, though, that even in flat space-time with the usual Minkowski coordinates, it's possible to have a set of geodesics which depart linearly away from each other, due to differences in initial velocity.So perhaps this may have been a long exercise in semantics.