Jeff Reid said:
I realize the Earth is spheroidal, but is its suface really equipotential as described in the attached images (ignoring surface issues like mountains)?
Yes and no.
The "no" response first: That equation is not correct. A quick check shows that it cannot be right. It implies that
\frac 1 {R_p} = \frac 1 {R_e} + \frac 1 2\,\frac{(R_e\Omega)^2}{\mu}
Plugging in the known values for the Earth's equatorial radius (6,378.137 km), the Earth's rotation rate (2*pi/23.9344696 hours), and the Earth's gravitational parameter (398,600.4418 km
3/s
2) yields a polar radius of 6367.1 km, and that is far from the mark. The correct value is 6,356.752 km.
The problem here is that the equation in that attached image implicitly assumes a spherical Earth by having potential as μ/r. The whole point of this exercise is to find out why the Earth is not spherical. A better model for the gravitational potential at some point on or above the surface of the Earth that accounts for the Earth's oblateness is
\Phi(r,\lambda) =<br />
\frac{\mu}{r}\left(<br />
1-J_2 \left(\frac{R_e} r\right)^2 \frac{3\sin^2\lambda - 1} 2<br />
\right)
where
- r is the distance of the point in question from the center of the Earth,
- λ is the geocentric (not geodetic) latitude of the point in question, and
- J2 is the first non-spherical term in the spherical harmonics expansion of gravitational potential. For the Earth J2=0.00108263.
With this, the expression for the Earth's polar radius becomes
\frac 1 {R_p}\left(1-J_2\left(\frac{R_e}{R_p}\right)^2\right) =<br />
\frac 1 {R_e}\left(1+\frac{J_2}2\right) + \frac 1 2\,\frac{(R_e\Omega)^2}{\mu}
Solving this for the Earth's polar radius yields 6356.743 km. The accepted value is 6,356.752 km, so now the error is all of 9 meters. Compare this to 10 kilometer error that results from ignoring Earth's oblateness.Now the "yes" response: The Earth's surface is an equipotential surface of gravitational potential plus centrifugal potential.
Although not commonly used for gravity, potential is commonly used for electrical fields and electric potential uses the unit "volt".
Gravitational potential is used for gravity in several regimes. The best models for the Earth's gravitational field are spherical harmonics expansions of the Earth's gravitational potential. Some of the more recent models:
EGM96 (Earth gravity model, 1996), a 360x360 spherical harmonics model of the Earth's potential, see
http://cddis.nasa.gov/926/egm96/egm96.html.
GGM02C (GRACE gravity model 02 constrained), a 200x200 spherical harmonics model of the Earth's potential, see
http://www.csr.utexas.edu/grace/gravity/
EGM2008 (Earth gravity model, 2008), a 2190x2159 spherical harmonics model of the Earth's potential, see
http://earth-info.nga.mil/GandG/wgs84/gravitymod/egm2008/index.html