An exoplanet survey reports the following for a newly characterised rocky planet:…

PHYSICS · Multi-part · Fermi University Physics · Relativity & Gravitation · Earth, Climate & Energy Physics · The solid Earth: structure, fields and thermal history

The Solid Earth, Ch The shape and gravity of the Earth: potential, geoid, isostasy and flexure

Problem

An exoplanet survey reports the following for a newly characterised rocky planet: equatorial radius a=6.00×106 ma = 6.00\times10^{6}\,\mathrm{m}, GM=3.00×1014 m3 s−2GM = 3.00\times10^{14}\,\mathrm{m^3\,s^{-2}}, rotation period T=18.0 hoursT = 18.0\,\mathrm{hours}, dynamical form factor J2=4.50×10−3J_2 = 4.50\times10^{-3} (from the satellite orbit) and dynamical ellipticity (C−A)/C=1/71.0(C-A)/C = 1/71.0 (from a measured precession rate). A separate radar-altimetry survey gives the planet's flattening directly as f=1/98.7f = 1/98.7. ((a)) Compute the rotational parameter m=ω2a3/GMm = \omega^2a^3/GM. ((b)) Use Clairaut's theorem, f=32J2+12mf = \tfrac32J_2 + \tfrac12m, to predict the flattening, and check it against the surveyed value. ((c)) Use MacCullagh's formula together with J2J_2 and (C−A)/C(C-A)/C to find C/Ma2C/Ma^2. ((d)) Use the Darwin-Radau relation with the surveyed ff and mm to find the value of C/Ma2C/Ma^2 a hydrostatic planet with this shape and spin would need. Compare it with part (c) and say whether this planet can be close to hydrostatic equilibrium.

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