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What's wrong with the obvious definition?Fredrik said:I don't think "spacelike geodesic" makes sense.
What's wrong with the obvious definition?Fredrik said:I don't think "spacelike geodesic" makes sense.
I don't know. Maybe nothing. What's the obvious definition?Hurkyl said:What's wrong with the obvious definition?
But I wasn't considering the length of just any path by looking at how long it was, I was specifically considering a spacelike path which lies in a single SR surface of simultaneity (the same surface that the straight-line path lies in). Is ds^2 = dx^2 + dy^2 + dz^2 - c^2dt^2 for this path not just equal to the spatial length of the path in the frame that uses this definition of simultaneity? After all, in the coordinate system where the path lies on a single surface of simultaneity, dt will always be zero. If that's right, that would be an argument to suggest why a geodesic doesn't maximize ds for spacelike paths, but that's OK because you said it minimized it.pmb_phy said:You're using Euclidean intuition in a Minkowski geometry. You can't determine the length of a worldine merely by looking at how long it is. E.g. for a time like worldline a squiggly path connecting two events has a smaller value of proper time than a straight worldline between the two.
Yes, but for timelike geodesics, a geodesic is not supposed to minimize [tex]\sqrt{-ds^2}[/tex] integrated along it, it's supposed to maximize it. My argument about connecting two events by a path consisting of two null geodesics was meant to show why I didn't think ds integrated along a spacelike path would be minimized. But maybe the answer has something to do with Hurkyl's distinction between being a "local optimum" and a "global optimum of the arclength function".pmb_phy said:Regarding your example of null geodesics. Its possible to connect any two events on a timelike geodesic by two straight null geodesics.
pmb_phy said:This is altogether different. Parallel transport has nothing to do with proper distance.jostpuur said:I suppose it's the usual: You need to do parallel transporting to compare velocities at different space time points. The relative velocity depends on the chosen path of parallel transport.pmb_phy said:What justification do you have for this assertion?Hurkyl said:In general relativity, we cannot even define what it means for things at two different locations in space-time to be at rest with each other, so "observer at rest with the mesaured object" is, strictly speaking, nonsense.
JesseM said:This isn't like SR where there is a preferred way to construct an observer's "rest frame" based on the fact that there's a special set of coordinate systems where the laws of physics take the same form, in GR all coordinate systems are on equal footing as far as physics is concerned, no?
This is true for timelike paths, but pmb_phy seems to say it's the opposite for spacelike paths. And as I said, it seems to me that if you look at two events with a spacelike separation and draw a squiggly path between them which lies entirely in the surface of simultaneity which contains both, this will have a greater spatial length (in the inertial coordinate system which defines simultaneity this way) than a straight-line path (which also lies within this surface of simultaneity). And in the inertial coordinate system where this surface of simultaneity has constant t, then dt is going to be 0 for every line element on the path, so ds^2 = dx^2 + dy^2 + dz^2 - c^2dt^2 reduces to ds^2 = dx^2 + dy^2 + dz^2, so the spatial length of the path in this coordinate system is the same as ds integrated along the path.MeJennifer said:In a Minkowski spacetime a geodesic is defined as the longest path between two events not the shortest path.
I was referring to the statement you made, i.e.JesseM said:But I wasn't considering the length of just any path by looking at how long it was, ...
What did you mean by "longer"?a squiggly path between two points has a greater length than a straight-line path.
The proper distance is defined for such a path, yes.I was specifically considering a spacelike path which lies in a single SR surface of simultaneity (the same surface that the straight-line path lies in). Is ds^2 = dx^2 + dy^2 + dz^2 - c^2dt^2 for this path not just equal to the spatial length of the path in the frame that uses this definition of simultaneity?
To be precise, a geodesic is a worldline for which "s" has a stationary value.After all, in the coordinate system where the path lies on a single surface of simultaneity, dt will always be zero. If that's right, that would be an argument to suggest why a geodesic doesn't maximize ds for spacelike paths, but that's OK because you said it minimized it.
I was merely giving you an example of a timelike geodesic for which events can be connected by two null worldlines.Yes, but for timelike geodesics, a geodesic is not supposed to minimize [tex]\sqrt{-ds^2}[/tex] integrated along it, it's supposed to maximize it.
Very minor point here, the proper length along constant t' is 0.8. I think you missed a square root. I only mention it because I was careful to pick numbers for which the square root worked out nicely :/Fredrik said:So the proper length along a path of constant t' is 0.64 (if we take v to be 0.6).
Fredrik said:Things get a lot more complicated in GR, so I'm not at all convinced that there's a way to get around the problem there. I would have to see a proof to believe that there is.
JesseM said:This is true for timelike paths, but pmb_phy seems to say it's the opposite for spacelike paths. And as I said, it seems to me that if you look at two events with a spacelike separation and draw a squiggly path between them which lies entirely in the surface of simultaneity which contains both, this will have a greater spatial length...
There are two equivalent definitions of a geodesic. One is, as you've said, a curve which parallel transports its tangent, the other is a curve which has a stationary value for its "length". Each is, equivalently, a more general definition.gel said:A spacelike geodesic neither minimizes nor maximizes the length, even locally. Which you can see by perturbing it in either a timelike or spacelike direction. However its length will be stationary (to first order under small perturbations). In any case, a geodesic is defined more generally as a curve which parallelly transports its own tangent vector.
pmb_phy said:There are two equivalent definitions of a geodesic. One is, as you've said, a curve which parallel transports its tangent, the other is a curve which has a stationary value for its "length". Each is, equivalently, a more general definition.
However I could likewise say that geodesics require only the concept of a metric to be defined. This can be defined by an affine connection but only requires the existence of a metric, which makes it the more general definition. :)gel said:when I said "more generally" I was referring to the fact that geodesics only require the concept of parallel transport to be defined. This can be defined by a metric, but only requires the existence of a connection, which makes it the more general definition.
I think if you looked at the context of that quote, you can see I was talking about a squiggly path through the surface of simultaneity which contained both events:pmb_phy said:I was referring to the statement you made, i.e.
What did you mean by "longer"?a squiggly path between two points has a greater length than a straight-line path.
In that context, I just meant having a longer spatial length in the coordinate system which used that definition of simultaneity.On the other hand, the straight-line path in flat spacetime also doesn't seem to maximize the value of ds integrated along it, since the value of ds integrated along a spacelike path is just the length of the path in the surface of simultaneity that contains it, and obviously in a given surface of simultaneity, a squiggly path between two points has a greater length than a straight-line path.
Does this mean that all small perturbations to the path change s in the same way, i.e. for a given path, either all small perturbations increase s, or else all small perturbations decrease s? (as suggested by Chris Hillman's post here) If so, is it possible to come up with examples of timelike paths where all small perturbations increase s (increase the proper time), or examples of spacelike paths where all small perturbations decrease s? Or do all timelike geodesics maximize the proper time with respect to small perturbations, and all spacelike geodesics minimize the length with respect to small perturbations? This review paper does seem to say that spacelike geodesics minimize s in some sense, in section 2.2, if I'm interpreting the language correctly:pmb_phy said:To be precise, a geodesic is a worldline for which "s" has a stationary value.
2.2. Special properties of geodesics in spacetimes depending
on their causal character. We will mean by co–spacelike any geodesic such
that the orthogonal of its velocity is a spacelike subspace at each point, that is: all
the geodesics in the Riemannian case and timelike geodesics in the Lorentzian one.
...
Timelike and co–spacelike geodesics. It is well known that conjugate points
along a timelike (resp. Riemannian) geodesic in a Lorentzian (resp. Riemannian)
manifold cannot have points of accumulation. Even more:
(1) Any timelike geodesic maximizes locally d in a similar way as any Riemannian
geodesic minimizes locally its corresponding d. Nevertheless, there are two
important differences:
– Riemannian geodesics minimize locally length among all the smooth
curves connecting two fixed points p, q. Nevertheless, the timelike ones
maximize only among the causal curves connecting p, q;
JesseM said:Yes, but for timelike geodesics, a geodesic is not supposed to minimize [tex]\sqrt{-ds^2}[/tex] integrated along it, it's supposed to maximize it.
You didn't give an example, just stated that it would be possible to do so--but anyway, I agree (you just need an event C between A and B such that A is on the past light cone of C and B is on the future light cone of C). Still, as I said, my argument was trying to show that there could always be a path with smaller s, whereas for timelike geodesics my understanding was that the geodesic maximizes s, at least compared to small perturbations. But perhaps the answer here is that this 0-s path is not itself a spacelike path, and it's possible to find a separate spacelike path which is minimal with respect to small perturbations?pmb_phy said:I was merely giving you an example of a timelike geodesic for which events can be connected by two null worldlines.
pmb_phy said:However I could likewise say that geodesics require only the concept of a metric to be defined. This can be defined by an affine connection but only requires the existence of a metric, which makes it the more general definition. :)
Pete
That the metric determines the connection is of no relevance in determining whether the metric or the connection provides a more general definition of geodesic. If it were the the metric would be more general since the connection canbe obtained from it.gel said:no, a metric defines a connection, but not the converse.
gel said:by more general, I mean it applies in more situations, even those where there isn't a metric.
pmb_phy said:And by more general I could say that it applies in more situations, even those where there isn't a connection.
I say I could say it. I didn't say I could prove it. :) That's why I asked you what are the "more cases" that you're referring to? From your response it seems that they are unrelated to geodesics.gel said:Could you? How would it do that?
Sorry but I'm not familiar with Lie groups. Would a geodesic even have a meaning in that case?You can define connections on Lie groups without any need for a metric. I think some approaches to quantum gravity use non-metric connections.
It just struck me what's going on.Fredrik said:I don't think "spacelike geodesic" makes sense.
That's right. That was a mistake by me. What my argument shows (I think) is that the alternative definition of a geodesic fails under certain conditions, but my argument isn't a problem for the standard definition.Hurkyl said:It just stuick me what's going on.
You were thinking local optima of paths -- which doesn't work here because the metric is not positive definite. For a spacelike path, a 'spatial perturbation' increases length, and a 'temporal perturbation' decreases length. Therefore, you saw a big problem with the notion of geodesic.
I was thinking unit vectors and parallel transport -- which still works here. Therefore, I didn't see any problem at all!
D'oh. I noticed that I got a different result than you, but I thought the mistake was on your end. You're right though. I calculated [itex]ds^2[/itex], not [itex]\sqrt{ds^2}[/itex].gel said:Very minor point here, the proper length along constant t' is 0.8. I think you missed a square root. I only mention it because I was careful to pick numbers for which the square root worked out nicely :/
Yes. Let's consider the Euclidean unit circle.pmb_phy said:Can you think of a case where one can define a geodesic but for which a metric cannot be defined?
Let me get back to you on this at a later date.Hurkyl said:Conclusion: this geometry cannot be expressed by a metric.
Because I have proven that parallel transport is not an isometry.pmb_phy said:Why?
What does it mean for parallel transport is not an isometry?Hurkyl said:Because I have proven that parallel transport is not an isometry.