rieman zeta
- 10
- 0
How does one compute the tidal locking radius of say a planet on a putative moon its area?
Is there a formula?
rieman zeta
Is there a formula?
rieman zeta
The tidal locking radius of a planet or moon can be computed using a specific formula derived from Burn's chapter in "Satellites" (U of Az Press). The formula is T = 16 rho omega a^6 (Q/k2) / (45 G M^2), where rho is the density of the body, omega is the initial rotation rate, a is the semi-major axis, Q/k2 is the dissipation function divided by the second order Love number, and M is the mass of the body doing the despinning. This formula demonstrates that the time constant for tidal locking is dependent on the mass and distance of the bodies involved, specifically showing an a^6/M^2 relationship. Understanding this relationship is crucial for calculating tidal locking timescales accurately.
PREREQUISITESAstronomers, astrophysicists, and planetary scientists interested in the dynamics of tidal locking and its implications for celestial body interactions.
Both you and Geoffrey have rightly commented on my poorly-defined
variables, so let me re-state this. BTW, I'm cribbing this formula (very
slightly modified) from somewhere else, namely Burn's chapter in
"Satellites" (U of Az Press), edited by Burns & Mathews:
T = 16 rho omega a^6 (Q/k2) / ( 45 G M^2 )
rho = density of body being despun [kg/m^3]
omega = inital rotation rate of body being despun [rad/s]
= 2 pi / P, where P is the inital rotation rate
a = semi-major axis of orbit [m]
Q/k2 = dissipation function divided by the 2nd order Love #
M = mass of body doing the despinning [kg]
I hope this is clearer - I've taken the formula for the despinning
timescale out of Burn's chapter and modified it very slightly.