Abstract

Aims.We aim to determine far-infrared fluxes at 70, 100, and 160μm for the five major Uranus satellites, Titania, Oberon, Umbriel, Ariel, and Miranda. Our study is based on the available calibration observations at wavelengths taken with the PACS photometer aboard theHerschelSpace Observatory.Methods.The bright image of Uranus was subtracted using a scaled Uranus point spread function (PSF) reference established from all maps of each wavelength in an iterative process removing the superimposed moons. The photometry of the satellites was performed using PSF photometry. Thermophysical models of the icy moons were fitted to the photometry of each measurement epoch and auxiliary data at shorter wavelengths.Results.The best-fit thermophysical models provide constraints for important properties of the moons, such as surface roughness and thermal inertia. We present the first thermal infrared radiometry longward of 50μm for the four largest Uranian moons, Titania, Oberon, Umbriel, and Ariel, at epochs with equator-on illumination. Due to this inclination geometry, heat transport took place to the night side so that thermal inertia played a role, allowing us to constrain that parameter. Also, we found some indication for differences in the thermal properties of leading and trailing hemispheres. The total combined flux contribution of the four major moons relative to Uranus is 5.7 × 10−3, 4.8 × 10−3, and 3.4 × 10−3at 70, 100, and 160μm, respectively. We therefore precisely specify the systematic error of the Uranus flux by its moons when Uranus is used as a far-infrared prime flux calibrator. Miranda is considerably fainter and always close to Uranus, impeding reliable photometry.Conclusions.We successfully demonstrate an image processing technique for PACS photometer data that allows us to remove a bright central source and reconstruct point source fluxes on the order of 10−3of the central source as close as ≈3 × the half width at half maximum of the PSF. We established improved thermophysical models of the five major Uranus satellites. Our derived thermal inertia values resemble those of trans-neptunian object (TNO) dwarf planets, Pluto and Haumea, more than those of smaller TNOs and Centaurs at heliocentric distances of about 30 AU.

Highlights

  • The planet Uranus is a well suited primary flux standard at the upper end of the accessible flux range for a number of contemporary far-infrared space and airborne photometers, such as ISOPHOT (Lemke et al 1996), Herschel-PACS (Poglitsch et al 2010), and HAWC+ (Harper et al 2018)

  • Our derived thermal inertia values resemble those of trans-neptunian object (TNO) dwarf planets, Pluto and Haumea, more than those of smaller TNOs and Centaurs at heliocentric distances of about 30 AORkey hemisp. UsefulSpectrum (AU)

  • How do the derived properties for the Uranian satellites compare with thermal inertias of other satellites and distant trans-neptunian objects (TNOs)? Lellouch et al (2013) analysed a large sample of TNOs and found a Γ = 2.5 ± 0.5 J m−2 s−1/2 K−1 for objects at heliocentric distances of rhelio = 20–50 AU

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Summary

Introduction

The planet Uranus is a well suited primary flux standard at the upper end of the accessible flux range for a number of contemporary far-infrared space and airborne photometers, such as ISOPHOT (Lemke et al 1996), Herschel-PACS (Poglitsch et al 2010), and HAWC+ (Harper et al 2018). With a detailed comparison of the Uranus image with a PACS reference point spread function (PSF; Fig. 1 middle), it is possible to trace extra features on top of the Uranus PSF. That is how we recognised the two largest and most distant of the five major Uranian moons, Titania and Oberon, in the PACS maps. We describe the method used to generate the Uranus reference PSF and subtract it from the maps in order to extract FIR fluxes for all five major moons of Uranus. This photometry will be compared with the thermophysical modelling of the moons

Input maps for Uranus PSF reference
Establishment of the Uranus reference PSFs
Median images
PSF matching
PSF subtraction
Maps of the Uranian moons
Photometry of the Uranian moons
PSF photometry
Aperture photometry
Photometry results
Auxiliary thermal data
Thermophysical modelling of the Uranian moons
Oberon
Titania
Umbriel
Miranda
Findings
Discussion
Conclusions

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