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Evolution of linear perturbations in spherically symmetric dust spacetimes

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abstract

We present results from a numerical code implementing a new method to solve the master equations describing the evolution of linear perturbations in a spherically symmetric but inhomogeneous background. This method can be used to simulate several configurations of physical interest, such as relativistic corrections to structure formation, the lensing of gravitational waves and the evolution of perturbations in a cosmological void model. This paper focuses on the latter problem, i.e. structure formation in a Hubble scale void in the linear regime. This is considerably more complicated than linear perturbations of a homogeneous and isotropic background because the inhomogeneous background leads to coupling between density perturbations and rotational modes of the spacetime geometry, as well as gravitational waves. Previous analyses of this problem ignored this coupling in the hope that the approximation does not affect the overall dynamics of structure formation in such models. We show that for a giga-parsec void, the evolution of the density contrast is well approximated by the previously studied decoupled evolution only for very large-scale modes. However, the evolution of the gravitational potentials within the void is inaccurate at more than the $10\%$ level, and is even worse on small scales.

fields

gr-qc 1

years

2019 1

verdicts

REJECT 1

representative citing papers

Propagation of Gravitational Waves in Anisotropic Universe

gr-qc · 2019-08-14 · reject · novelty 3.0

In a toy anisotropic universe, gravitational waves acquire direction-dependent dispersion relations and anisotropy-dependent tidal acceleration, but the background equations contain a sign error that undermines the model.

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  • Propagation of Gravitational Waves in Anisotropic Universe gr-qc · 2019-08-14 · reject · none · ref 45 · internal anchor

    In a toy anisotropic universe, gravitational waves acquire direction-dependent dispersion relations and anisotropy-dependent tidal acceleration, but the background equations contain a sign error that undermines the model.