No evidence of magma ocean on Io based on Juno/JIRAM data

Fuente: arXiv
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Autores principales: Tosi, Federico, Mura, Alessandro, Zambon, Francesca
Formato: Preprint
Publicado: 2024
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author Tosi, Federico
Mura, Alessandro
Zambon, Francesca
author_facet Tosi, Federico
Mura, Alessandro
Zambon, Francesca
contents A recent paper (ref. 1) used infrared images of Io acquired by the Juno/JIRAM instrument to derive a latitudinal dependence of the spectral radiance and conclude that such latitudinal dependence is consistent with a magma ocean model. We challenge their conclusions, and we draw attention to some potential issues with their analysis. In this letter, we will use three arguments to show that: (1) the (ref. 1) paper uses saturated data; (2) the M-filter of the JIRAM imager is only a weak and incomplete proxy for the total power output; and finally (3) even assuming that the radiance was correctly estimated, the latitudinal dependence of the 4.8-$μ$m spectral radiance is not statistically significant. These facts, taken together, demonstrate that the results presented in (ref. 1) are not sufficient to confirm consistency with a magma ocean model on Io.
format Preprint
id arxiv_https___arxiv_org_abs_2412_04321
institution arXiv
publishDate 2024
record_format arxiv
spellingShingle No evidence of magma ocean on Io based on Juno/JIRAM data
Tosi, Federico
Mura, Alessandro
Zambon, Francesca
Earth and Planetary Astrophysics
Instrumentation and Methods for Astrophysics
A recent paper (ref. 1) used infrared images of Io acquired by the Juno/JIRAM instrument to derive a latitudinal dependence of the spectral radiance and conclude that such latitudinal dependence is consistent with a magma ocean model. We challenge their conclusions, and we draw attention to some potential issues with their analysis. In this letter, we will use three arguments to show that: (1) the (ref. 1) paper uses saturated data; (2) the M-filter of the JIRAM imager is only a weak and incomplete proxy for the total power output; and finally (3) even assuming that the radiance was correctly estimated, the latitudinal dependence of the 4.8-$μ$m spectral radiance is not statistically significant. These facts, taken together, demonstrate that the results presented in (ref. 1) are not sufficient to confirm consistency with a magma ocean model on Io.
title No evidence of magma ocean on Io based on Juno/JIRAM data
topic Earth and Planetary Astrophysics
Instrumentation and Methods for Astrophysics
url https://arxiv.org/abs/2412.04321