Analytical model of tidal distortion and dissipation for a giant planet with a viscoelastic core
NI Storch, D Lai - Monthly Notices of the Royal Astronomical …, 2015 - academic.oup.com
NI Storch, D Lai
Monthly Notices of the Royal Astronomical Society, 2015•academic.oup.comWe present analytical expressions for the tidal Love numbers of a giant planet with a solid
core and a fluid envelope. We model the core as a uniform, incompressible, elastic solid,
and the envelope as a non-viscous fluid satisfying the n= 1 polytropic equation of state. We
discuss how the Love numbers depend on the size, density, and shear modulus of the core.
We then model the core as a viscoelastic Maxwell solid and compute the tidal dissipation
rate in the planet as characterized by the imaginary part of the Love number k 2. Our results …
core and a fluid envelope. We model the core as a uniform, incompressible, elastic solid,
and the envelope as a non-viscous fluid satisfying the n= 1 polytropic equation of state. We
discuss how the Love numbers depend on the size, density, and shear modulus of the core.
We then model the core as a viscoelastic Maxwell solid and compute the tidal dissipation
rate in the planet as characterized by the imaginary part of the Love number k 2. Our results …
Abstract
We present analytical expressions for the tidal Love numbers of a giant planet with a solid core and a fluid envelope. We model the core as a uniform, incompressible, elastic solid, and the envelope as a non-viscous fluid satisfying the n = 1 polytropic equation of state. We discuss how the Love numbers depend on the size, density, and shear modulus of the core. We then model the core as a viscoelastic Maxwell solid and compute the tidal dissipation rate in the planet as characterized by the imaginary part of the Love number k2. Our results improve upon existing calculations based on planetary models with a solid core and a uniform (n = 0) envelope. Our analytical expressions for the Love numbers can be applied to study tidal distortion and viscoelastic dissipation of giant planets with solid cores of various rheological properties, and our general method can be extended to study tidal distortion/dissipation of super-Earths.
Oxford University Press