Does General Relativity theory correctly explain the ellipsoidal shape of the earth?
It seems it does not because the Thirring expression¹ for the force of a spherical shell—of mass $M$, radius $R$, and spinning at $\vec{\Omega}$—on an internal test particle of mass $m$ at $\vec{r}$, $$\vec{F}=-\frac{4GM}{15Rc^2}\left[\color{red}{2m\left(\vec{\Omega}\cdot\vec{r}\right)\vec{\Omega}}+\color{green}{m\vec{\Omega}\times\left(\vec{\Omega}\times\vec{r}\right)}+5\cdot\color{blue}{2m\left(\vec{v}\times\vec{\Omega}\right)}\right],$$ his terms differing from those of the most general Newtonian expression for fictitious forces acting on a particle moving in a rotating, non-inertial frame: $$\vec{F}_f=\color{green}{m\vec{\omega}\times\left(\vec{\omega}\times\vec{r'}\right)}-\color{blue}{2m\left(\vec{\omega}\times\vec{v'}\right)}-m\frac{d\vec{\omega}}{dt}\times\vec{r'}-m\frac{d^2\vec{h}}{dt^2},$$$\vec{h}$ being the displacement between the inertial and non-inertial frames, the third term being Euler's force, and the last term being the fictitious "force of inertia."³
Thus, Thirring predicts:
- an additional fictitious force that has no equivalent in Newton's theory: $\color{red}{m\left(\vec{\Omega}\cdot\vec{r}\right)\vec{\Omega}}$;
- the coefficient of the centrifugal term, $\color{green}{m\vec{\Omega}\times\left(\vec{\Omega}\times\vec{r}\right)}$, is 5× smaller than that of the Coriolis term, $\color{blue}{2m\left(\vec{v}\times\vec{\Omega}\right)}$; but in Newton's theory, the coefficients are equal.
This would seem to greatly affect how GR explains the ellipsoidal shape of the earth.
References:
Mashhoon, Bahram, Friedrich W. Hehl, and Dietmar S. Theiss. “On the Gravitational Effects of Rotating Masses: The Thirring-Lense Papers.” General Relativity and Gravitation 16, no. 8 (August 1, 1984): 711–50. doi:10.1007/BF00762913.
Assis, André K. T. Relational Mechanics and Implementation of Mach’s Principle with Weber’s Gravitational Force. Apeiron, 2014. p. 293 (PDF p. 313), equations (16.16) and (16.17). For the application of this to the earth's flattening, see §16.5.2, pp. 298-300 (PDF pp. 318-20).
Symon, Keith R. Mechanics. Reading, Mass.: Addison-Wesley Pub. Co., 1971. ch. 7.
Lanczos, Cornelius. The Variational Principles of Mechanics. Toronto: University of Toronto Press, 1970. ch. IV, §§4-5.