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Analytical Model of Tidal Distortion and Dissipation for a Giant Planet with a Viscoelastic Core
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 n...
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description | 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 \(k_2\). 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. |
doi_str_mv | 10.48550/arxiv.1502.06550 |
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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 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.</description><identifier>EISSN: 2331-8422</identifier><identifier>DOI: 10.48550/arxiv.1502.06550</identifier><language>eng</language><publisher>Ithaca: Cornell University Library, arXiv.org</publisher><subject>Computational fluid dynamics ; Distortion ; Equations of state ; Exact solutions ; Extrasolar planets ; Fluid flow ; Incompressible flow ; Jupiter ; Love number ; Mathematical analysis ; Mathematical models ; Rheological properties ; Saturn ; Shear modulus ; Viscoelasticity ; Viscous fluids</subject><ispartof>arXiv.org, 2015-02</ispartof><rights>2015. This work is published under http://arxiv.org/licenses/nonexclusive-distrib/1.0/ (the “License”). 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subjects | Computational fluid dynamics Distortion Equations of state Exact solutions Extrasolar planets Fluid flow Incompressible flow Jupiter Love number Mathematical analysis Mathematical models Rheological properties Saturn Shear modulus Viscoelasticity Viscous fluids |
title | Analytical Model of Tidal Distortion and Dissipation for a Giant Planet with a Viscoelastic Core |
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