arXiv subjects

R. Sordini

Publications and source records attributed to R. Sordini.

5 recordsLinked to original sources

arXiv2026

Analysis of Io's tidal response as a function of the properties of the partially molten layer

Io's internal heat is generated by Jupiter-driven tidal dissipation and Laplace resonance. This energy partially melts the mantle, but the melt fraction, depth, and spatial distribution of dissipation remain poorly constrained. Tidal deformation is linked to the mantle's physical state via a parametric approach accounting for melting onset depth and latent heat of fusion. Io is modeled as a three-layer body comprising a fluid core, a viscoelastic mantle, and an elastic lithosphere. The degree-2 potential Love number k2 is computed by solving spheroidal oscillation equations with an adapted California Planetary Geophysics Code (CPGC). Mantle properties (viscosity, shear modulus, Andrade parameter beta) are iteratively updated based on the local melt fraction, and mantle compressibility is explicitly incorporated. Results show a self-consistent shallow-mantle enhancement of tidal heating. Melt presence decreases effective viscosity and increases anelasticity, amplifying upper-mantle dissipation. Reproducing the observed real part of k2 in 1D models requires melt fractions below the rheologically critical threshold. Compressibility yields higher values for the real part of k2, reinforcing this upper bound. Mass flux analysis confirms melt percolation capacity exceeds thermodynamic production, implying efficient drainage. The reference Andrade parameter beta strongly influences the imaginary Love numbers (k2, h2, l2) and the predicted libration amplitude. These constraints support a heterogeneous mantle characterized by a magmatic sponge structure rather than a global magma ocean, establishing a quantitative framework linking Io's interior, partial melting, and tidal dissipation to Juno observations.

astro-ph.EP↗

arXiv2025

Synchronized Eruptions on Io: Evidence of Interconnected Subsurface Magma Reservoirs

On December 27, 2024, Juno's JIRAM infrared experiment observed an unprecedented volcanic event on Io's southern hemisphere, covering a vast region of ~ 65,000 square km, near 73{\deg}S, 140{\deg}E. The total power output is estimated between 140 and 260 TW, potentially the most intense ever recorded, surpassing the brightest eruption at Surt in 2001 (~80 TW). Within that region, only one hot spot was previously known (Pfd454). This feature was earlier estimated to cover an area of 300 square km with a total power output of 34 GW. JIRAM results show that the region produces a power output of 140-260 TW, over 1,000 times higher than earlier estimates. Three adjacent hot spots also exhibited dramatic power increases: P139, PV18, and an unnamed feature south of the main one that surged to ~1 TW, placing all of them among the top 10 most powerful hot spots observed on Io. A temperature analysis of the features supports a simultaneous onset of these brightenings and suggests a single eruptive event propagating beneath the surface across hundreds of kilometers, the first time this has been observed on Io. This implies a connection among the hotspots' magma reservoirs, while other nearby hotspots that have been known to be active in the recent past, such as Kurdalagon Patera, appear unaffected. The simultaneity supports models of massive, interconnected magma reservoirs. The global scale of this event involving multiple hotspots and covering several hundred thousand square km should be considered in the future models of the lithosphere and interior of Io.

astro-ph.EP↗

arXiv2024

Vertical and temporal H3+ structure at the auroral footprint of Io

We report the first observation of the vertical and temporal structure of the H3+ emission at the auroral footprint of Io, as observed by Juno/JIRAM. The brightness vertical profile shows a maximum at 600 km above 1 bar, with no apparent difference between the Main Alfvén Wing spot emission and the tail of the footprint. This observation is more compatible with a broadband energy distribution of the precipitating electrons, than a monoenergetic one. The temporal profile of H3+ column density has been observed after the passage of the MAW and shows a hyperbolic decrease. A model of H3+ decay is proposed, which takes into account the second-order kinetic of dissociative recombination of H3+ ions with electrons. The model is found to be in very good agreement with Juno observation. The conversion factor from radiance to column density has been derived, as well as the half-life for H3+, which is not constant but inversely proportional to the H3+ column density. This explains the wide range of H3+ lifetimes proposed before.

astro-ph.EP↗

arXiv2012

Intensity and polarization of the atmospheric emission at millimetric wavelengths at Dome Concordia

Atmospheric emission is a dominant source of disturbance in ground-based astronomy at mm wavelengths. The Antarctic plateau is recognized to be an ideal site for mm and sub-mm observations, and the French/Italian base of Dome C is among the best sites on Earth for these observations. In this paper we present measurements, performed using the BRAIN-pathfinder experiment, at Dome C of the atmospheric emission in intensity and polarization at 150GHz, one of the best observational frequencies for CMB observations when considering cosmic signal intensity, atmospheric transmission, detectors sensitivity, and foreground removal. Careful characterization of the air-mass synchronous emission has been performed, acquiring more that 380 elevation scans (i.e. "skydip") during the third BRAIN-pathfinder summer campaign in December 2009/January 2010. The extremely high transparency of the Antarctic atmosphere over Dome Concordia is proven by the very low measured optical depth: =0.050 \pm 0.003 \pm 0.011 where the first error is statistical and the second is systematic error. Mid term stability, over the summer campaign, of the atmosphere emission has also been studied. Adapting the radiative transfer atmosphere emission model "am" to the particular conditions found at Dome C, we also infer the level of the PWV content of the atmosphere, notoriously the main source of disturbance in millimetric astronomy ( =0.77 +/- 0.06 + 0.15 - 0.12 mm). Upper limits on the air-mass correlated polarized signal are also placed for the first time. The degree of circular polarization of atmospheric emission is found to be lower than 0.2% (95%CL), while the degree of linear polarization is found to be lower than 0.1% (95%CL). These limits include signal-correlated instrumental spurious polarization.

astro-ph.IM↗

arXiv2010

QUBIC: The QU Bolometric Interferometer for Cosmology

One of the major challenges of modern cosmology is the detection of B-mode polarization anisotropies in the CMB. These originate from tensor fluctuations of the metric produced during the inflationary phase. Their detection would therefore constitute a major step towards understanding the primordial Universe. The expected level of these anisotropies is however so small that it requires a new generation of instruments with high sensitivity and extremely good control of systematic effects. We propose the QUBIC instrument based on the novel concept of bolometric interferometry, bringing together the sensitivity advantages of bolometric detectors with the systematics effects advantages of interferometry. Methods: The instrument will directly observe the sky through an array of entry horns whose signals will be combined together using an optical combiner. The whole set-up is located inside a cryostat. Polarization modulation will be achieved using a rotating half-wave plate and interference fringes will be imaged on two focal planes (separated by a polarizing grid) tiled with bolometers. We show that QUBIC can be considered as a synthetic imager, exactly similar to a usual imager but with a synthesized beam formed by the array of entry horns. Scanning the sky provides an additional modulation of the signal and improve the sky coverage shape. The usual techniques of map-making and power spectrum estimation can then be applied. We show that the sensitivity of such an instrument is comparable with that of an imager with the same number of horns. We anticipate a low level of beam-related systematics thanks to the fact that the synthesized beam is determined by the location of the primary horns. Other systematics should be under good control thanks to an autocalibration technique, specific to our concept, that will permit the accurate determination of most of the systematics parameters.

astro-ph.IM↗