lpetrich
Science Advisor
- 998
- 180
Because of how accurate it's been possible to make atomic clocks, we now face a similar problem here on the Earth's surface and low Earth orbit, especially with the Global Positioning Satellites (GPS).
First, there's the question of the definition of time in general relativity, with its curved space-time. Viable GR alternatives like Generalized Brans-Dicke feature the same sort of curvature, but with different source terms, so this discussion will carry over into them. Every entity has its own proper time, but that alone gives us no way of relating them. Instead, one must define time in a way that gives every space-time point a well-defined time. Thus, time is defined from a foliation or splitting up of space-time into spacelike 3-hypersurfaces, where each hypersurface has a time value associated with it. For flat space-time, it is easy. The standard definition of time there involves flat and parallel 3-hypersurfaces, with time changing at constant rate in an orthogonal direction. Most GR definitions try to approximate that definition to within the limits of space-time curvaure. If there is a time-translation symmetry, as with the Schwarzschild and Kerr black-hole solutions, then one can use it to define an overall time. Likewise, the FLRW cosmology metric has a well-defined overall time in it.
Our Galaxy, like the Earth and its neighborhood, are well within the weak-field limit, so one must use a post-Newtonian expansion to define a standard foliation and a time coordinate. But there seems to be a generally-accepted foliation, one that makes the space-time metric look like the usual statement of the Parametrized Post-Newtonian metric. It's close to the flat-spacetime one.
But those preliminaries aside, let us look at Earth timekeeping.
Astronomers started out by using the Earth's rotation, but the orbits of the Moon and the planets showed variations that were closely parallel, so they switched to Ephemeris Time, the time associated with those orbits. The Earth's rotation's irregularities is what those variations were. Then in the 1960's, humanity had gotten laboratory clocks that could compete with astronomical measurements: atomic clocks. They now use as a reference International Atomic Time (TAI, from its French initials), kept by some 300 atomic clocks in some 30 national laboratories. Their measured times are compared to each other to get a more precise standard than any individual one.
TAI is intended as a realization of Terrestrial Time (English and French initials the same), the time at the Earth's sea-level surface (the "geoid").
This time can be extrapolated to infinity relative to the Earth while ignoring other objects, yielding Geocentric Coordinate Time (TCG). It flows faster than TT does, with an additional factor of 7.0*10-10, meaning that clocks at infinity would look fast by that additional factor relative to the Earth's surface. That's about 22 milliseconds/year.
One can do the same with the Earth and the Solar System. Its Barycentric Coordinate Time (TCB) flows faster than Earth-surface time by an additional factor of about 1.6*10-8. That's about half a second per year.
Doing that with the Solar System and our Galaxy yields an additional factor of about 10-6 for extragalactic vs. Solar-System time. That's about 30 seconds/year. Over a century, that adds up to about an hour.
So time-rate variations within our Galaxy are not going to be very noticeable unless one does very precise timekeeping.
First, there's the question of the definition of time in general relativity, with its curved space-time. Viable GR alternatives like Generalized Brans-Dicke feature the same sort of curvature, but with different source terms, so this discussion will carry over into them. Every entity has its own proper time, but that alone gives us no way of relating them. Instead, one must define time in a way that gives every space-time point a well-defined time. Thus, time is defined from a foliation or splitting up of space-time into spacelike 3-hypersurfaces, where each hypersurface has a time value associated with it. For flat space-time, it is easy. The standard definition of time there involves flat and parallel 3-hypersurfaces, with time changing at constant rate in an orthogonal direction. Most GR definitions try to approximate that definition to within the limits of space-time curvaure. If there is a time-translation symmetry, as with the Schwarzschild and Kerr black-hole solutions, then one can use it to define an overall time. Likewise, the FLRW cosmology metric has a well-defined overall time in it.
Our Galaxy, like the Earth and its neighborhood, are well within the weak-field limit, so one must use a post-Newtonian expansion to define a standard foliation and a time coordinate. But there seems to be a generally-accepted foliation, one that makes the space-time metric look like the usual statement of the Parametrized Post-Newtonian metric. It's close to the flat-spacetime one.
But those preliminaries aside, let us look at Earth timekeeping.
Astronomers started out by using the Earth's rotation, but the orbits of the Moon and the planets showed variations that were closely parallel, so they switched to Ephemeris Time, the time associated with those orbits. The Earth's rotation's irregularities is what those variations were. Then in the 1960's, humanity had gotten laboratory clocks that could compete with astronomical measurements: atomic clocks. They now use as a reference International Atomic Time (TAI, from its French initials), kept by some 300 atomic clocks in some 30 national laboratories. Their measured times are compared to each other to get a more precise standard than any individual one.
TAI is intended as a realization of Terrestrial Time (English and French initials the same), the time at the Earth's sea-level surface (the "geoid").
This time can be extrapolated to infinity relative to the Earth while ignoring other objects, yielding Geocentric Coordinate Time (TCG). It flows faster than TT does, with an additional factor of 7.0*10-10, meaning that clocks at infinity would look fast by that additional factor relative to the Earth's surface. That's about 22 milliseconds/year.
One can do the same with the Earth and the Solar System. Its Barycentric Coordinate Time (TCB) flows faster than Earth-surface time by an additional factor of about 1.6*10-8. That's about half a second per year.
Doing that with the Solar System and our Galaxy yields an additional factor of about 10-6 for extragalactic vs. Solar-System time. That's about 30 seconds/year. Over a century, that adds up to about an hour.
So time-rate variations within our Galaxy are not going to be very noticeable unless one does very precise timekeeping.
