Evidence for local acceleration of heavy >10 MeV/n oxygen and sulphur in Jupiter's innermost radiation belts

2021 ◽  
Author(s):  
Elias Roussos ◽  
Christina Cohen ◽  
Peter Kollmann ◽  
Marco Pinto ◽  
Patricia Gonçalves ◽  
...  

<p>Jupiter's radiation belts constitute a multi-component system, trapping high intensities of electrons, protons and heavier ions. We revisit measurements from Galileo's Heavy Ion Counter (HIC) instrument, a high-quality dataset that extends considerably the energy range covered by Galileo/EPD and Juno/JEDI (<10 MeV/n) up to ~100 MeV/n, providing key complementary observations for those two instruments in the equatorial radiation belts. Thanks to HIC's large geometry factor and event-based measurement capabilities, the instrument clearly resolves trace ions of both heliospheric and magnetospheric origin, such as Carbon, Nitrogen, Sodium, Magnesium, Iron and others, besides the much more abundant Oxygen and Sulfur. In this work we re-evaluate aspects of HIC's calibration, particularly for the analysis of measurements obtained at the innermost, intense radiation belts of Jupiter, which are currently monitored by Juno. We concentrate on previously unpublished observations from Galileo's last two orbits, reaching inward of Amalthea's orbit, including a close flyby of this moon. We show that the structure and composition of the heavy ion belts depends strongly on energy, L-shell and pitch angle. We find that above 50 MeV/n, Jupiter's heavy ion radiation belts are dominated by oxygen, appearing stable and are highly structured by strong losses at the orbits of Io, Thebe and Amalthea, a structure reminiscent of that observed in Saturn's proton radiation belts. In addition, heavy ion spectra and the corresponding phase space density profiles indicate that a local source of energy exists at least inward of Amalthea, accelerating oxygen above 100 MeV/n and sulphur above ˜50 MeV/n. Between the orbits of Io and Amalthea, PSD profiles indicate contributions from local and adiabatic acceleration for both ion species, with the former dominating at the highest energies resolved in that region (˜50 MeV/n). In conclusion, unlike Earth's radiation belts, where the highest energy protons or ions observed reach the terrestrial magnetosphere pre-accelerated to the MeV range in the form of solar, anomalous or galactic cosmic rays, Jupiter can efficiently accelerate oxygen and sulphur, which originate at at eV energies at Io and its torus, by 7-8 decades in energy.</p>

1984 ◽  
Vol 46 (10) ◽  
pp. 885-893 ◽  
Author(s):  
T Nygrén ◽  
L Jalonen ◽  
A Huuskonen ◽  
T Turunen

2019 ◽  
Vol 66 (1) ◽  
pp. 177-183
Author(s):  
Zhenyu Wu ◽  
Shuming Chen ◽  
Jianjun Chen ◽  
Pengcheng Huang

2003 ◽  
Vol 30 (20) ◽  
Author(s):  
D. Santos‐Costa ◽  
M. Blanc ◽  
S. Maurice ◽  
S. J. Bolton

2017 ◽  
Vol 44 (11) ◽  
pp. 5259-5268 ◽  
Author(s):  
P. Kollmann ◽  
C. Paranicas ◽  
G. Clark ◽  
B. H. Mauk ◽  
D. K. Haggerty ◽  
...  

2019 ◽  
Vol 489 (5) ◽  
pp. 502-505
Author(s):  
V. B. Lapshin ◽  
M. S. Ivanov ◽  
N. G. Kotonaeva ◽  
V. A. Burov ◽  
A. Yu. Repin

A scenario is proposed for replenishing the Earths exosphere with atomic hydrogen of cosmic origin. An assessment was made and the coincidence of the total atomic hydrogen content in the exosphere with the number of protons (after thermolization converted into hydrogen ions) precipitated in the SAA zone during the year according to the data of the Meteor M and NOAA‑19 satellites was confirmed. The observed coincidence indicates that the rates of replenishment of hydrogen due to precipitation from radiation belts and dissipation into outer space coincide in order of magnitude. It is concluded that the exosphere hydrogen is mainly of cosmic origin and its main source is the thermalized protons of galactic cosmic rays, solar cosmic rays and partially solar wind.


Author(s):  
M. E. Wiedenbeck ◽  
W. R. Binns ◽  
A. C. Cummings ◽  
A. J. Davis ◽  
G. A. de Nolfo ◽  
...  

2018 ◽  
Vol 8 ◽  
pp. A06 ◽  
Author(s):  
Sigiava Aminalragia-Giamini ◽  
Ingmar Sandberg ◽  
Constantinos Papadimitriou ◽  
Ioannis A. Daglis ◽  
Piers Jiggens

A new probabilistic model introducing a novel paradigm for the modelling of the solar proton environment at 1 AU is presented. The virtual enhancements − solar proton event radiation model (VESPER) uses the European space agency's solar energetic particle environment modelling (SEPEM) Reference Dataset and produces virtual time-series of proton differential fluxes. In this regard it fundamentally diverges from the approach of existing SPE models that are based on probabilistic descriptions of SPE macroscopic characteristics such as peak flux and cumulative fluence. It is shown that VESPER reproduces well the dataset characteristics it uses, and further comparisons with existing models are made with respect to their results. The production of time-series as the main output of the model opens a straightforward way for the calculation of solar proton radiation effects in terms of time-series and the pairing with effects caused by trapped radiation and galactic cosmic rays.


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