Model-independent reconstruction of the linear anisotropic stress $η$
Ana Marta Pinho, Santiago Casas, Luca Amendola
TL;DR
The paper develops a model-independent estimator for the linear anisotropic stress eta, named eta_obs, based on H(z), E_g, and fσ8 data to test gravity without strong model assumptions. It introduces three reconstruction methods—binning, Gaussian Process, and polynomial regression—to recover E(z), P2, and P3 from sparse data and hence eta_obs. Across redshifts around 0.3–0.86, the methods yield eta_obs values that are broadly compatible within 1σ; the fiducial polynomial regression result is 0.49±0.69, while the other methods show mild tensions. The authors advocate polynomial regression as the most robust approach and anticipate much tighter tests with upcoming surveys such as Euclid.
Abstract
In this work, we use recent data on the Hubble expansion rate $H(z)$, the quantity $fσ_8(z)$ from redshift space distortions and the statistic $E_g$ from clustering and lensing observables to constrain in a model-independent way the linear anisotropic stress parameter $η$. This estimate is free of assumptions about initial conditions, bias, the abundance of dark matter and the background expansion. We denote this observable estimator as $η_{\rm obs}$. If $η_{\rm obs}$ turns out to be different from unity, it would imply either a modification of gravity or a non-perfect fluid form of dark energy clustering at sub-horizon scales. Using three different methods to reconstruct the underlying model from data, we report the value of $η_{\rm obs}$ at three redshift values, $z=0.29, 0.58, 0.86$. Using the method of polynomial regression, we find $η_{\rm obs}=0.57\pm1.05$, $η_{\rm obs}=0.48\pm0.96$, and $η_{\rm obs}=-0.11\pm3.21$, respectively. Assuming a constant $η_{\rm obs}$ in this range, we find $η_{\rm obs}=0.49\pm0.69$. We consider this method as our fiducial result, for reasons clarified in the text. The other two methods give for a constant anisotropic stress $η_{\rm obs}=0.15\pm0.27$ (binning) and $η_{\rm obs}=0.53 \pm 0.19$ (Gaussian Process). We find that all three estimates are compatible with each other within their $1σ$ error bars. While the polynomial regression method is compatible with standard gravity, the other two methods are in tension with it.
