New Polarimetric Data for the Galilean Satellites: Io and Ganymede Observations and Modeling

New high-precision disk-integrated measurements of the polarization of Io and Ganymede in the UBVRI bands are presented. The observations were obtained using polarimeters mounted on the Crimean Astrophysical Observatory and the Peak Terskol Observatory in 2019–2023. For Io, the negative polarization...

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Main Authors: Nikolai Kiselev, Vera Rosenbush, Ari Leppälä, Karri Muinonen, Ludmilla Kolokolova, Aleksandr Savushkin, Nikolai Karpov
Format: Article
Language:English
Published: IOP Publishing 2024-01-01
Series:The Planetary Science Journal
Subjects:
Online Access:https://doi.org/10.3847/PSJ/ad0bf9
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author Nikolai Kiselev
Vera Rosenbush
Ari Leppälä
Karri Muinonen
Ludmilla Kolokolova
Aleksandr Savushkin
Nikolai Karpov
author_facet Nikolai Kiselev
Vera Rosenbush
Ari Leppälä
Karri Muinonen
Ludmilla Kolokolova
Aleksandr Savushkin
Nikolai Karpov
author_sort Nikolai Kiselev
collection DOAJ
description New high-precision disk-integrated measurements of the polarization of Io and Ganymede in the UBVRI bands are presented. The observations were obtained using polarimeters mounted on the Crimean Astrophysical Observatory and the Peak Terskol Observatory in 2019–2023. For Io, the negative polarization branch (NPB) reaches a minimum of P _min ≈ −0.25 ± 0.02% in the V band at a phase angle of α _min = 2.°1 ± 0.°5. The inversion angle is α _inv = 26° ± 6° in the V and R bands. The NPB for Ganymede is an asymmetric curve, with P _min = −0.34 ± 0.01% at α _min = 0.°52 ± 0.°06 and α _inv = 8.°5 ± 0.°2 in the V band. Although Io and Europa have similar geometric albedos (0.63 and 0.67, respectively), their NPB shapes differ. The NPB of Ganymede (albedo of 0.43) is morphologically similar to that of Europa, although it is described by different parameter values ( P _min , α _min , and α _inv ). This discrepancy is likely due to the compositions of their surfaces: Europa’s with H _2 O ice, Io’s with sulfuric/silicate composition, and Ganymede’s with H _2 O ice and silicates. Numerical computations using the radiative transfer coherent backscattering method demonstrated a match to the polarimetric observations and to the geometric albedos for Ganymede with the single-scattering albedo ≈ 0.943 and mean free path length kl = 2 πl / λ _eff ≈ 150, where λ _eff is the wavelength. For Io’s regolith, the single-scattering albedo was found to be ≈ 0.979 and kl ≈ 40.
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spelling doaj.art-f88e0e7bcb024c218bb0f7f0bc139de22024-01-18T13:31:25ZengIOP PublishingThe Planetary Science Journal2632-33382024-01-01511010.3847/PSJ/ad0bf9New Polarimetric Data for the Galilean Satellites: Io and Ganymede Observations and ModelingNikolai Kiselev0https://orcid.org/0000-0002-2451-4079Vera Rosenbush1https://orcid.org/0000-0002-2353-2451Ari Leppälä2https://orcid.org/0009-0008-7221-1671Karri Muinonen3https://orcid.org/0000-0001-8058-2642Ludmilla Kolokolova4https://orcid.org/0000-0002-9321-3202Aleksandr Savushkin5Nikolai Karpov6Crimean Astrophysical Observatory, Nauchnij, 298409, CrimeaTaras Shevchenko National University of Kyiv , Astronomical Observatory, 04053 Kyiv, Ukraine; Main Astronomical Observatory of National Academy of Sciences of Ukraine, 03143 Kyiv, UkraineUniversity of Helsinki , Department of Physics, Helsinki, Finland ; ari.leppala@helsinki.fiUniversity of Helsinki , Department of Physics, Helsinki, Finland ; ari.leppala@helsinki.fiUniversity of Maryland , College Park, MD 20742, USACrimean Astrophysical Observatory, Nauchnij, 298409, CrimeaInternational Center for Astronomical, Medical and Ecological Research, Peak Terskol Observatory, UkraineNew high-precision disk-integrated measurements of the polarization of Io and Ganymede in the UBVRI bands are presented. The observations were obtained using polarimeters mounted on the Crimean Astrophysical Observatory and the Peak Terskol Observatory in 2019–2023. For Io, the negative polarization branch (NPB) reaches a minimum of P _min ≈ −0.25 ± 0.02% in the V band at a phase angle of α _min = 2.°1 ± 0.°5. The inversion angle is α _inv = 26° ± 6° in the V and R bands. The NPB for Ganymede is an asymmetric curve, with P _min = −0.34 ± 0.01% at α _min = 0.°52 ± 0.°06 and α _inv = 8.°5 ± 0.°2 in the V band. Although Io and Europa have similar geometric albedos (0.63 and 0.67, respectively), their NPB shapes differ. The NPB of Ganymede (albedo of 0.43) is morphologically similar to that of Europa, although it is described by different parameter values ( P _min , α _min , and α _inv ). This discrepancy is likely due to the compositions of their surfaces: Europa’s with H _2 O ice, Io’s with sulfuric/silicate composition, and Ganymede’s with H _2 O ice and silicates. Numerical computations using the radiative transfer coherent backscattering method demonstrated a match to the polarimetric observations and to the geometric albedos for Ganymede with the single-scattering albedo ≈ 0.943 and mean free path length kl = 2 πl / λ _eff ≈ 150, where λ _eff is the wavelength. For Io’s regolith, the single-scattering albedo was found to be ≈ 0.979 and kl ≈ 40.https://doi.org/10.3847/PSJ/ad0bf9Planetary scienceSolar system astronomy
spellingShingle Nikolai Kiselev
Vera Rosenbush
Ari Leppälä
Karri Muinonen
Ludmilla Kolokolova
Aleksandr Savushkin
Nikolai Karpov
New Polarimetric Data for the Galilean Satellites: Io and Ganymede Observations and Modeling
The Planetary Science Journal
Planetary science
Solar system astronomy
title New Polarimetric Data for the Galilean Satellites: Io and Ganymede Observations and Modeling
title_full New Polarimetric Data for the Galilean Satellites: Io and Ganymede Observations and Modeling
title_fullStr New Polarimetric Data for the Galilean Satellites: Io and Ganymede Observations and Modeling
title_full_unstemmed New Polarimetric Data for the Galilean Satellites: Io and Ganymede Observations and Modeling
title_short New Polarimetric Data for the Galilean Satellites: Io and Ganymede Observations and Modeling
title_sort new polarimetric data for the galilean satellites io and ganymede observations and modeling
topic Planetary science
Solar system astronomy
url https://doi.org/10.3847/PSJ/ad0bf9
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