Consider a clock aboard a satellite orbiting the Earth, such as a Global Positioning System (GPS) transmitter. There are two major relativistic influences upon its rate of timekeeping: a special relativistic correction for its orbital speed and a general relativistic correction for its orbital altitude. Both of these effects can be treated at an introductory level, making for an appealing application of relativity to everyday life.

1.
For example, see D.C. Giancoli, Physics for Scientists and Engineers, 3rd ed. (Prentice Hall, Upper Saddle River, NJ, 2000), Chap. 37.
2.
The relativistic kinetic energy of a body is defined as K ≡ E − E0, where E0 is the body's rest energy. In the case of a photon, E0 = 0 so that E = K.
3.
I.R. Kenyon, General Relativity (Oxford Univ. Press, Oxford, 1990), Chap. 2. These approximate methods of deriving Eq. (2) agree with an exact general relativistic treatment, presented in an accessible manner in E.F. Taylor and J.A. Wheeler, “Project A: Global Positioning System,” in Exploring Black Holes: Introduction to General Relativity (Addison-Wesley, San Francisco, 2000), pp. A-1–A-9.
4.
E. Huggins, “GPS satellites and Lagrangians,” presented at the AAPT Summer Meeting, Madison, WI, 2003. Equation (3) implies that the action per unit mass for an orbiting clock is equal to the time lost multiplied by the speed of light squared.
5.
N.
Ashby
, “
Relativity and the Global Positioning System
,”
Phys. Today
55
,
41
47
(May
2002
).
Also see N. Ashby, “Relativity in the Global Positioning System,” Living Reviews in Relativity6 (Jan. 2003), online at http://www.livingreviews.org/lrr-2003-1.
6.
A.
Harvey
and
E.
Schucking
, “
A small puzzle from 1905
,”
Phys. Today
58
,
34
36
(March
2005
).
Also see
S. P.
Drake
, “
The equivalence principle as a stepping stone from special to general relativity: A Socratic dialog
,”
Am. J. Phys.
74
,
22
25
(Jan.
2006
).
7.
Specifically, in Earth's rotating frame of reference the total surface potential is computed as follows. The gravitational potential difference in Eq. (5) is gy for small altitudes y above polar sea level. The centripetal acceleration of an object revolving with angular speed ω at a distance r from the axis is ω2r. (For the Earth, ω = 2π/24 h.) In a rotating frame, this can be treated as an outward centrifugal acceleration. Its integral corresponds to a centrifugal potential of 12ω2r2 = −12υ2. If we now require that the total potential gy − υ2/2 = 0 everywhere on Earth's surface, then Eqs. (1) and (5) cancel each other's effects. [Note, however, that ω2rE2/2g = 11 km is half the height of Earth's actual equatorial bulge, as discussed in standard texts such as D.L. Turcotte and G. Schubert, Geodynamics, 2nd ed. (Cambridge Univ. Press, Cambridge, 2002), Chap. 5. In fact, an equatorial clock needs to be raised beyond 11 km to compensate for the gravitational field from the mass of the bulge.]
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