Abstract

Context. We address the issue of remote sensing of the surfaces of Galilean icy moons. We investigate the prospects for retrieval of the physical parameters of the surface of the Jovian icy moons from submillimeter wave radiometry data. Aims. We show that the model parameters could not be completely retrieved from the polarized radiometry data, but some of their combinations can be effectively constrained. Methods. The polarized radiative transfer in lossy porous ice was numerically simulated. A Bayesian maximum likelihood retrieval algorithm was developed and tested on the simulated data in a wide range of variation of the model parameters. The uncertainty of the retrievals was evaluated with the Cramer-Rao bounds. We established the combinations of model parameters that can be effectively constrained from the measured data. Results. We reveal that the effective scatterer size can be reliably constrained for a range of values where the scattering asymmetry parameter uniquely depends on the wave parameter, and for relatively high values of the single scattering albedo, for which the scattering in the medium is significant. Similarly, the domains of reliable retrieval of the single scattering albedo and thermal skin depth are established.

Highlights

  • The Galilean icy moons (Greenberg 2010) differ from most objects of the Solar System in several respects

  • Radar echoes coming from the Galilean satellites, which indicated high reflectivity and anomalous polarization signatures (Ostro & Shoemaker 1990; Black et al 2001a), have been interpreted and explained with different theoretical models

  • The secondary objective of this study is to investigate the thermal radiation polarization, and its role and importance for the retrievals

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Summary

Introduction

The Galilean icy moons (Greenberg 2010) differ from most objects of the Solar System in several respects. In addition to remarkably high reflectance in the optical (Buratti 1985) and microwave spectrum (Black et al 2001a,b), they exhibit anomalous polarization signatures of radar echoes (Black et al 2001b; Campbell 2012), which are not typical for most planetary surfaces. For this reason, many studies address the issues of their structure, composition, and thermal regime. Radar echoes coming from the Galilean satellites, which indicated high reflectivity and anomalous polarization signatures (Ostro & Shoemaker 1990; Black et al 2001a), have been interpreted and explained with different theoretical models

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