Is the Surface of a Sphere Locally Flat?

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Discussion Overview

The discussion revolves around the concept of local flatness on the surface of a sphere, specifically examining the conditions under which a manifold can be considered Euclidean at a point and the implications of coordinate choice on the metric. Participants explore theoretical aspects of differential geometry and the behavior of metrics in different coordinate systems.

Discussion Character

  • Technical explanation
  • Debate/contested
  • Mathematical reasoning

Main Points Raised

  • One participant describes a scenario involving the metric of a sphere and questions the validity of their teacher's explanation regarding local flatness and coordinate choice.
  • Another participant suggests that the issue arises from selecting inappropriate coordinates, emphasizing that the existence of Euclidean coordinates is contingent on the choice made.
  • A different viewpoint asserts that once the metric is set to be Euclidean at a point, the coordinates become fixed, limiting the options for other coordinate systems.
  • Some participants propose that polar coordinates with the equator passing through the point of interest can resolve the issue of non-zero first-order corrections.
  • There is a discussion about the flexibility of coordinate systems, with one participant arguing that multiple Cartesian coordinates can exist and that rotations of axes are permissible.
  • Another participant clarifies that the inability to conceive of alternative coordinates does not imply their non-existence, highlighting the nature of coordinate transformations and their effects on the metric tensor.
  • Miscommunication regarding language and expression is noted, with a participant reflecting on how their phrasing may have led to misunderstandings about their level of knowledge.

Areas of Agreement / Disagreement

Participants express differing views on the implications of coordinate choice for local flatness and the existence of alternative coordinate systems. There is no consensus on the resolution of the original question regarding the teacher's explanation.

Contextual Notes

Participants acknowledge the complexity of the topic, including the dependence on specific coordinate choices and the implications for the metric's behavior in the vicinity of a point. The discussion highlights the nuances in defining local flatness and the role of coordinate transformations in differential geometry.

Jufa
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TL;DR
Something our teacher explained me regarding the metric and local flatness doesn't match a simple example of a sphere
Given a certain manifold in ##R^3## I've been told that at every location ##p## it is possible to encounter a reference frame from which the metric is the euclidean at zero order from that point and its first correction is of second order. This, nevertheless does not match with the following example:
Consider the surface of a sphere ##S^2## at a certain polar angle ##\theta_0## and azimutal angle ##\phi_0##. The metric of that surface is
##g_{\phi \phi} = sin^2(\theta) ## and ##g_{\theta \theta} = 1##. Let as define a new local reference frame such that ##\theta' = \theta## and ##\phi' = \frac{\phi}{sin(\theta_0)}##. It is easy to see that the new metric in this reference frame will be euclidean at ##p##. But what happens in its neighbourhood?

##g_{\phi \phi} = \frac{sin^2(\theta_0 + \delta \theta)}{sin^2(\theta_0} = 1 + 2sin(\theta_0)cos(\theta_0)\delta \theta + cos^2(\theta_0)(\delta \theta)^2##

which clearly has a non-vanishing correction at first order.

Where is the problem? Is my teacher wrong?
Thanks in advance.
 
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Jufa said:
Summary:: Something our teacher explained me regarding the metric and local flatness doesn't match a simple example of a sphere

Where is the problem?
You picked the wrong coordinates. The statement is just that those coordinates exists where the metric is Euclidean to zeroth order around p and the first correction is at order two, not that this will be the case whatever coordinates you pick.
 
Orodruin said:
You picked the wrong coordinates. The statement is just that those coordinates exists where the metric is Euclidean to zeroth order around p and the first correction is at order two, not that this will be the case whatever coordinates you pick.
I can't imagine a set of coordinates that fulfills the non-zero first order correction condition. Indeed, once you impose that the metric is euclidean at p, the new coordinates become fixed and, thus, my choice was the only one possible to be made.
 
Jufa said:
I can't imagine a set of coordinates that fulfills the non-zero order condition.
Polar coordinates with the equator passing through your location should do the trick.
 
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Jufa said:
But what happens in its neighbourhood?

##g_{\phi \phi} = \frac{sin^2(\theta_0 + \delta \theta)}{sin^2(\theta_0} = 1 + 2sin(\theta_0)\delta \theta + (\delta \theta)^2##

which clearly has a non-vanishing correction at first order.

Where is the problem? Is my teacher wrong?
As @Orodruin mentioned you just picked bad coordinates, and as @Ibix mentioned (people are fast on this forum!) you can just use standard coordinates with the equator going through the point of interest. However, in general you can always construct such coordinates even if they have nothing to do with some original starting coordinates.
 
Ibix said:
Polar coordinates with the equator passing through your location should do the trick.

That definitely solves it. Many thanks!
 
Jufa said:
once you impose that the metric is euclidean at p, the new coordinates become fixed

No, they don't. There is more than one possible set of Cartesian coordinates; you can rotate the axes any way you like.
 
Dale said:
As @Orodruin mentioned you just picked bad coordinates, and as @Ibix mentioned (people are fast on this forum!) you can just use standard coordinates with the equator going through the point of interest. However, in general you can always construct such coordinates even if they have nothing to do with some original starting coordinates.
Sure, I only mention the first set of coordinates in order to define the metric tensor.
 
Jufa said:
I can't imagine a set of coordinates that fulfills the non-zero first order correction condition. Indeed, once you impose that the metric is euclidean at p, the new coordinates become fixed and, thus, my choice was the only one possible to be made.
That you cannot imagine a different set of coordinates does not mean it doesn't exist. It is fairly simple to see that having orthonormal basis vectors at one point does not fix the coordinate system, not only because you can always rotate your coordinates, but also because any coordinate change for which ##\partial x^a/\partial y^b = \delta^a_b## at the point of interest will not change the components of the metric tensor. Furthermore, among those coordinate changes you can find one that makes the Christoffel symbols vanish at that point because the coordinate change of the Christoffel symbols also depends on the second derivatives of the coordinate change functions, which are not fixed by fixing the metric components.
 
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  • #10
I know it. I did not mean that the fact that I cannot imagine it means that it does not exist. I was just expressing my ignorance of such a coordinates system.
Thanks.
 
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Jufa said:
I know it. I did not mean that the fact that I cannot imagine it means that it does not exist. I was just expressing my ignorance of such a coordinates system.
I'm guessing English isn't your first language? Unfortunately, "I can't imagine that..." in English is usually taken to mean "It is impossible that...", which may have caused some miscommunication here. I think "I can't think of a set of coordinates..." would probably be closer to what you were aiming for. You could probably do with an "I think" somewhere in the second sentence of post #3 too, I'm afraid.
 

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