In the Schwarzchild metric, $t$ is the time on the clock of an observer at infinity, and $r$ is the related to the area of a sphere by $A=4\pi r^2$. Are there more physical coordinates one could use, where $t$ is the time on the clock of an observer at finite $r$, and $r$ refers to distances this observer could actually measure with a meter stick? I know the metric will depend on the motion of the observer, but perhaps there are some "preferred frames" that are more relevant than others?
1 Answers
"More physical" is a little vague, and depending on the precise meaning there are indeed other alternatives.
For instance, spatially isotropic coordinates exist: search for "isotropic coordinates" or check Buchdahl's paper, and take a look at this question.
A simple way for the time coordinate to reflect proper time for a static observer at a radius $r_0$ is simply to rescale the Scharzschild's metric $t$-coordinate by an appropriate amount $L$: $t' = Lt$.
This is what's actually done in the definition of Terrestrial Time TT coordinate, of which International Atomic Time TAI (and therefore Universal Coordinated Time UTC, besides leap seconds) is a realization:
For many Earth-related astronomy applications, the geocentric celestial reference system GCRS of coordinates $(T,X,Y,Z)$ is used. It is a truncated series expansion of isotropic coordinates for the Schwarzschild solution (outside the event horizon). Its time coordinate $T$ is called Geocentric Coordinate Time TCG, and represents the proper time of a non-rotating observer at infinity. Terrestrial time TT is related to TCG by a linear transformation, so that it equals the proper time measured (in an averaged sense) by a stationary observer on Earth's surface. The scaling in this linear transformation takes into account that the observer is not at infinity, and is moreover moving. For these matters see e.g.
Petit, Wolf: Relativistic theory for time comparisons: a review, especially § 3.4.
Kaplan: The IAU Resolutions on Astronomical Reference Systems, Time Scales, and Earth Rotation Models, chapter 2.
A similar rescaling can be done for the $r$ coordinate.
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