# Properties of Electrons Accelerated by the Ganymede-Magnetosphere Interaction: Survey of Juno High-Latitude Observations

J. Rabia, V. Hue, N. André, Q. Nénon, J. R. Szalay, F. Allegrini, A. H.

Sulaiman, C. K. Louis, T. K. Greathouse, Y. Sarkango, et al.

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## ► To cite this version:

J. Rabia, V. Hue, N. André, Q. Nénon, J. R. Szalay, et al., Properties of Electrons Accelerated by the Ganymede-Magnetosphere Interaction: Survey of Juno High-Latitude Observations. Journal of Geophysical Research Space Physics, 2024, 129 (5), 10.1029/2024JA032604. insu-04726502

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# JGR Space Physics

## RESEARCH ARTICLE

10.1029/2024JA032604

**Key Points:**

* Juno particle and UV measurements are combined with field-line tracing to identify 11 in situ crossings of the Ganymede flux tube

* We provide a statistical study of the accelerated electrons observed in the high-latitude far-field region

* We find two distinct regions in which the electrons properties, that is, characteristic energy, energy flux, and distribution, greatly differ

**Supporting Information:**

Supporting Information may be found in the online version of this article.

**Correspondence to:**

J. Rabia,
jonas.rabia@irap.omp.eu

**Citation:**

Rabia, J., Hue, V., André, N., Nénon, Q., Szalay, J. R., Allegrini, F., et al. (2024). Properties of electrons accelerated by the Ganymede-magnetosphere interaction: Survey of Juno high-latitude observations. *Journal of Geophysical Research: Space Physics*, 129, e2024JA032604. https://doi.org/10.1029/2024JA032604

Received 1 MAR 2024

Accepted 1 MAY 2024

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## Properties of Electrons Accelerated by the Ganymede-Magnetosphere Interaction: Survey of Juno High-Latitude Observations

J. Rabia¹ ID, V. Hue² ID, N. André¹,³ ID, Q. Nénon¹, J. R. Szalay⁴ ID, F. Allegrini⁵,⁶ ID, A. H. Sulaiman⁷ ID, C. K. Louis⁸ ID, T. K. Greathouse⁵ ID, Y. Sarkango⁴ ID, D. Santos-Costa⁵ ID, M. Blanc¹,² ID, E. Penou¹ ID, P. Louarn¹ ID, R. W. Ebert⁵,⁶ ID, G. R. Gladstone⁵,⁶ ID, A. Mura⁹ ID, J. E. P. Connerney¹⁰,¹¹ ID, and S. J. Bolton⁵ ID

¹Institut de Recherche en Astrophysique et Planétologie, CNRS-UPS-CNES, Toulouse, France, ²Aix-Marseille Université, CNRS-CNES, Institut Origines, LAM, Marseille, France, ³Institut Supérieur de l'Aéronautique et de l'Espace (ISAE-SUPAERO), Université de Toulouse, Toulouse, France, ⁴Department of Astrophysical Sciences, Princeton University, Princeton, NJ, USA, ⁵Southwest Research Institute, San Antonio, TX, USA, ⁶Department of Physics and Astronomy, University of Texas at San Antonio, San Antonio, TX, USA, ⁷School of Physics and Astronomy, Minnesota Institute for Astrophysics, University of Minnesota, Minneapolis, MN, USA, ⁸LESIA, Observatoire de Paris, Université PSL, CNRS, Sorbonne Université, Université de Paris, Meudon, France, ⁹Institute for Space Astrophysics and Planetology, National Institute for Astrophysics, Rome, Italy, ¹⁰NASA Goddard Space Flight Center, Greenbelt, MD, USA, ¹¹Space Research Corporation, Annapolis, MD, USA

**Abstract** The encounter between the Jovian co-rotating plasma and Ganymede gives rise to electromagnetic waves that propagate along the magnetic field lines and accelerate particles by resonant or non-resonant wave-particle interaction. They ultimately precipitate into Jupiter's atmosphere and trigger auroral emissions. In this study, we use Juno/JADE, Juno/UVS data, and magnetic field line tracing to characterize the properties of electrons accelerated by the Ganymede-magnetosphere interaction in the far-field region. We show that the precipitating energy flux exhibits an exponential decay as a function of downtail distance from the moon, with an e-folding value of 29°, consistent with previous UV observations from the Hubble Space Telescope (HST). We characterize the electron energy distributions and show that two distributions exist. Electrons creating the Main Alfvén Wing (MAW) spot and the auroral tail always have broadband distribution and a mean characteristic energy of 2.2 keV while in the region connected to the Transhemispheric Electron Beam (TEB) spot the electrons are distributed non-monotonically, with a higher characteristic energy above 10 keV. Based on the observation of bidirectional electron beams, we suggest that Juno was located within the acceleration region during the 11 observations reported. We thus estimate that the acceleration region is extended, at least, between an altitude of 0.5 and 1.3 Jupiter radius above the 1-bar surface. Finally, we estimate the size of the interaction region in the Ganymede orbital plane using far-field measurements. These observations provide important insights for the study of particle acceleration processes involved in moon-magnetosphere interactions.

**Plain Language Summary** The Galilean moons orbit in a plasma-rich environment, created by the intense volcanism of Io and transported radially outward in the Jovian magnetosphere. At the orbital locations of the moons, this plasma, co-rotating with Jupiter, flows at a velocity significantly higher than the moons' orbital speed. Consequently, the moons disturb the plasma flow. This interaction gives rise to a set of physical processes, including the generation of electromagnetic waves that propagate away from the moons and accelerate charged particles, triggering auroral emissions by precipitating into Jupiter's atmosphere. In this study, we investigate the properties of the electrons accelerated by the Ganymede-magnetosphere interaction. We use data from the JADE and UVS instruments onboard the Juno spacecraft as well as magnetic field line tracing methods. Following a statistical characterization of the electron properties, we compare our results with previous findings that have reported electron observations resulting from the Io- and Europa-magnetosphere interactions.
# 1. Introduction

The Juno mission (Bolton et al., 2017), in orbit around Jupiter since July 2016, is characterizing the auroral emissions and the accelerated particles that generate them with unprecedented temporal and spatial resolution. In particular, the study of the moons' auroral footprints and underlying physical processes is made possible by the highly eccentric orbit of the spacecraft, which enables Juno to cross the different moons magnetic flux shells several times per orbit. In situ measurements obtained across the magnetic field lines connecting the moons orbital locations to Jupiter's atmosphere reveal the diversity of physical processes occurring during the moon-magnetosphere interactions.

The most visible manifestation of these moon-magnetosphere interactions is the generation of UltraViolet (UV) and InfraRed (IR) auroral emissions at the feet of the connected magnetic field lines (Clarke et al., 1998, 2002; Connerney et al., 1993; Mura et al., 2017, 2018; Prangé et al., 1996). These auroral footprints are composed of a main spot, the Main Alfvén Wing (MAW) spot, that is linked to the respective moon Alfvén wings, followed by an auroral tail that extends in the direction of the magnetospheric plasma flow (Gérard et al., 2006). Depending on the location of the moons in the Jovian magnetodisc, a spot created by a Trans-hemispheric Electron Beam (TEB) can be observed upstream of the MAW spot or downstream of it (Bonfond et al., 2008). This TEB is created by electrons accelerated in the anti-Jovian direction in one hemisphere, traveling along the magnetic field line and precipitating into the opposite hemisphere.

The formation of these auroral structures is made possible by the generation in the moons local environments of electromagnetic waves that propagate away from the moons along the magnetic field lines as Alfvén waves, and accelerate particles. Such electromagnetic coupling between Jupiter and its moons was first predicted by Goldreich and Lynden-Bell (1969), and confirmed by Voyager 1 measurements at Io (Acuña et al., 1981). Theoretical formalisms were then developed to explain the propagation of Alfvén waves from the vicinity of the moons to Jupiter's auroral regions (Goertz, 1980; Gurnett & Goertz, 1981; Neubauer, 1980, 1998). More recently, these waves have been observed in situ by the Juno spacecraft (Sulaiman et al., 2020). Statistical studies have shown that the efficiency of the Alfvén waves-particles energy transfer is close to 10% (Sulaiman et al., 2023), consistent with an interaction between electrons and Alfvén waves filamented by turbulent cascade (Hess et al., 2010). Theoretical and modeling studies have also been carried out to understand the propagation of Alfvén waves and their role in the particle acceleration in Jupiter's magnetosphere (Coffin et al., 2022; Damiano et al., 2019; Jacobsen et al., 2007; Lysak et al., 2023; Saur et al., 2018), showing in particular that the energization due to non-resonant interaction with inertial Alfvén waves leads to broadband particle acceleration (Damiano et al., 2023). Resonant wave-particle interaction can occur when the length scale of waves becomes close to the electron inertial scale, allowing an energy transfer between the waves and the particles (Saur et al., 2018), which may happen close to Jupiter, in low-altitude regions.

Electron and proton broadband spectra have been reported in numerous Juno in situ observations, either in the auroral regions (Allegrini, Mauk, et al., 2020; Mauk et al., 2017) or in the moons' magnetic flux tubes (Clark et al., 2018, 2020; Rabia et al., 2023; Szalay, Bagenal, et al., 2020; Szalay et al., 2018, 2020a, 2020b), confirming the prominent role played by Alfvén waves to accelerate particles. Recently, Sarkango et al. (2024) also reported observations of banded proton and electron distributions within flux tubes connected to the Galilean moons, consistent with a resonant process between particles' bounce motion and standing Alfvén waves. However, Allegrini, Gladstone, et al. (2020) and Hue et al. (2022) have shown that electron spectra measured during crossings of two particular flux tubes of Europa and Ganymede, likely connected to their TEB spots, do not always exhibit a broadband distribution but rather a non-monotonic one with a peak in the Differential Number Flux (DNF) spectrum. Rabia et al. (2023) have demonstrated that, at Europa, a progressive transition occurs as a function of downward distance from the moon, from non-monotonic spectra first observed in the TEB flux tubes to broadband spectra observed farther down the tail. These observations suggest that other physical processes may occur during the electron acceleration in TEB flux tubes leading to modifications of their energy spectra.

Similarly, observations of UV footprints associated with the moon Enceladus (Pryor et al., 2011, 2024) and intense waves activity within its flux tubes (Sulaiman et al., 2018) have revealed that similar processes occur during moon-magnetosphere interactions at Saturn. However, the high-latitude properties of the particles accelerated during the Enceladus-magnetosphere interactions remain unknown, preventing any detailed comparisons with observations reported in Jupiter's magnetosphere.
In this study, we investigate the properties of electrons in Ganymede's flux tubes. We use a cross-correlation between Juno/JADE and Juno/UVS data to identify clear signatures of Ganymede-magnetosphere interactions in the far field regions, that is, at high latitude close to Jupiter. The instruments, the physical parameters derived from the data, and the methods used in this study are described in Section 2. The statistical properties of electrons in Ganymede's flux tubes are presented in Section 3. Finally, Section 4 and 5 discuss the results in the context of electron acceleration in the Ganymede-magnetosphere interaction, summarize the main conclusions, and offer perspectives for future works.

## 2. Methods

### 2.1. Considered Data Set

We use in situ measurements made by the JADE-E instrument (McComas et al., 2017) obtained above Jupiter's polar regions. In these regions, the JADE-E instrument can measure the properties of electrons initially between 50 eV and 100 keV at a 1-s cadence. This energy range was reduced to 32 eV–32 keV after PeriJove (PJ) 32. Thanks to its two sensors that provide each a 120°-field of view, a large fraction of the pitch angle distribution can be reconstructed, depending on the orientation of the spacecraft with respect to the local magnetic field. Pitch angles are derived using magnetic field directions obtained by the MAG instrument (Connerney et al., 2017).

The proximity of Ganymede's footprint with the main auroral oval, and the dynamics observed in the Jovian middle magnetosphere (Mauk et al., 2002) can make the identifications of Ganymede's flux tube crossings in the JADE data sometimes challenging. To overcome this difficulty, we used observations from the Juno/UVS instrument to cross-correlate the in situ and remote observations. UVS is an imaging spectrograph characterizing the Jovian auroral emission between 68 and 210 nm (Gladstone et al., 2017), and designed to provide context spectral images to the Juno in situ and remote sensing instruments. During the periJove observation phase, UVS scans the auroral region of Jupiter every 30 s. By co-adding consecutive images, it is possible to build up complete maps of the auroral regions (Bonfond, Gladstone, et al., 2017; Bonfond, Saur, et al., 2017; Greathouse et al., 2021). Because of the short lifetime of Jupiter's auroral structures, comparisons between the Juno in situ measurements and UVS imagery must be done with data recorded simultaneously.

IR images and spectra of the Ganymede footprint, taken from Juno, exist as well (Mura et al., 2017, 2018). However, the typical H3+ decay time, which is responsible for IR emission, is variable and can be between tens to a few hundred seconds. This causes the morphology of UV and IR footprints to be different (Gérard et al., 2018) and also makes instantaneous comparison of remote and in situ data impossible. In addition, the pointing flexibility offered by UVS scan mirror allows targeting specific auroral features, making the UVS satellite auroral footprint data set extensive (e.g., Hue et al., 2019; Hue et al., 2023). For this reason, we focused our study on the UV images of the Ganymede footprint.

We used here UV-false color images derived by spectrally binning the UVS data into three “color” channels. The red, green and blue channels account for the photons recorded by UVS in the 145–165 nm, 119–145 nm, and 70–119 nm ranges, respectively. The intensity of the red channel is a proxy for the electron characteristic energy, in a similar fashion as the traditional color ratio (Yung et al., 1982). That quantity uses the fact that the absorption cross-section of methane drops off sharply at wavelengths longer than 145 nm. The absorption of <145 nm UV auroral emissions from stratospheric methane increases with the depth of precipitating electrons, and therefore with the electron characteristic energy. Comparing the false color of the auroral features observed at the Juno footprint provides an additional way to correlate in situ with remote sensing measurements (Szalay et al., 2020a), instead of only looking at the Juno calculated M-shell from the magnetic mapping.

The satellite footprints result from the interaction between the co-rotating plasma and the moons. These spots therefore do not co-rotate with the planet and can be distinguished from other auroral emissions as their rotation rate follows the orbital motion of the moons. UVS spectral images were produced by co-adding a number of spins around the Ganymede flux tube crossing times (see, e.g., the method used in Hue et al., 2022). The UVS time window was optimized per case to produce an image co-added over a large-enough time window providing a complete picture of the auroral emissions near the footprints, but short enough to limit the smearing of the footprints.
## 2.2. Identification of the Crossings of the Ganymede Flux Tubes

In order to identify potential crossings of Ganymede's flux tubes by Juno in the JADE data obtained between PJ1 and PJ50, we apply the step-by-step method described hereafter.

1. We first rely on a magnetic field line tracing method to estimate when Juno magnetic footprint crossed the Ganymede footpath, that is, the location on the Jupiter poles of the magnetic field lines connected to Ganymede's orbital location. For this purpose, we used the JRM33 magnetic field model (Connerney et al., 2022) coupled to the CON2020 current sheet model (Connerney et al., 2020) since this combination gives the most accurate description of the magnetic field at the orbital locations of Io, Europa, and Ganymede (Rabia et al., 2024). The magnetic field lines are iteratively traced with a constant step size of 1/350 R<sub>j</sub> (1 R<sub>j</sub> = 71,492 km), that is, ~200 km, toward the auroral regions. We projected the position of Juno onto Jupiter's atmosphere at a 900 km-altitude, which corresponds to the mean altitude of the moon-induced UV aurora (Bonfond et al., 2009), and estimated the times when it crossed the predicted footpath of Ganymede. Altitudes are calculated above the 1-bar level. The footpaths of the moons considered, also derived using JRM33 + CON2020 model, are available in Connerney et al. (2022). A catalog of ~150 potential crossings is built, covering the Juno orbits between PJ1 and PJ50, corresponding to ~3 crossings per orbit.

2. We restrict the catalog to the cases where Juno's altitude is below 1.5 R<sub>j</sub> to ensure that the loss cone (LC) is sufficiently large to be resolved by the JADE-E instrument. Below this altitude, the LC is larger than 15°. This criterion also ensures that the Juno altitude is small enough to measure accelerated electrons, that is, that Juno's is below or within the acceleration region. This criterion excludes 40 cases of the catalog, 110 potential crossings of Ganymede's flux tubes remain.

3. We limit our catalog to the cases where Juno crossed the Ganymede footpath close to the Ganymede magnetic footprint. For this purpose, we add a criterion on the longitude separation between the magnetic footprint of Juno and the location of Ganymede MAW spot, that is, $-20° < \Delta\lambda_{Alfven} < 60°$ (see Section 2.3 for the definition of the $\Delta\lambda_{Alfven}$ metric), to ensure that electrons fluxes resulting from the Ganymede-magnetosphere interactions are sufficiently strong to be measured in situ above the background magnetospheric particle flux. Indeed, Bonfond, Saur, et al. (2017) estimated that Ganymede's UV tail has a length of ~24°, which provides a typical spatial scale over which the electron fluxes decreases. 23 potential crossings remains after this stage.

4. We analyze the UVS data for the 23 potential crossings identified. We discard the cases in which the Ganymede UV footprint and auroral tail are not clearly visible on the Jupiter pole and/or not distinguishable from nearby auroral emissions unrelated to satellite auroral emissions. We then analyze the time series of JADE-E measurements and correlate the in situ electron observations with their auroral counterparts observed by UVS along the footpath of Juno, as presented in Figures 1 and 2. By correlating the sequence of events observed in both instruments (see Section 3.1), we obtain 11 cases where we observe electrons accelerated by the Ganymede-magnetosphere interactions. A similar procedure was also used by Allegrini, Gladstone, et al. (2020) and Szalay et al. (2020a) to identify a Europa footprint crossing during PJ12N and a Ganymede MAW flux tube crossing during PJ20N, respectively. We emphasize that the 11 events reported in this study are the only ones to exhibit a clear acceleration signature in the JADE-E data.

## 2.3. Electron Properties Characterization

We characterize the electron properties by deriving the precipitating energy flux (EF) and the precipitating electron characteristic energy ($E_{char}$) using the formulas presented in Rabia et al. (2023). All the quantities presented hereafter are made using electron measurements within the loss cone, whose size is estimated based on the formula of Mauk et al. (2017).

In Section 3, the 11 crossings of the Ganymede's flux tubes identified are organized according to the $\Delta\lambda_{Alfven}$ separation, the angle along each moon's orbit between the moon and an Alfvén wave trajectory connected to the tail aurora (Szalay et al., 2020b), and where $\Delta\lambda_{Alfven} = 0°$ theoretically corresponds to the MAW spot. This metric takes into account the propagation of Alfvén waves from the close environment of the moons up to Jupiter's ionosphere and is based on an empirical model derived from UVS observations of the Io, Europa, and Ganymede MAW spots (Hue et al., 2023). By providing an estimate of the downtail separation from the MAW spot, previous studies at Io and Europa have shown that the $\Delta\lambda_{Alfven}$ metric is the most suitable parameter for organizing electron
fluxes as it allows to minimize the scatter of the *EF* downtail of the MAW (Rabia et al., 2023; Szalay et al., 2020b).

This $\Delta\lambda_{\text{Alfven}}$ separation allows to divide the observations into three regions depending on the $\Delta\lambda_{\text{Alfven}}$ separation, that is, TEB for $\Delta\lambda_{\text{Alfven}} < -3^\circ$, MAW for $-3^\circ < \Delta\lambda_{\text{Alfven}} < 3^\circ$, and auroral tail for $\Delta\lambda_{\text{Alfven}} > 3^\circ$. Indeed, since the $\Delta\lambda_{\text{Alfven}}$ metric quantifies the angular separation from the MAW spot, a negative $\Delta\lambda_{\text{Alfven}}$ value likely refers to the crossing of a structure upstream of the MAW, most likely the TEB. However, as this metric can be greatly affected by the time variability of the magnetospheric conditions (see Hue et al., 2023), for example, plasma density, magnetic field strength, magnetodisc scale height, we consider that the crossing occurring at $\Delta\lambda_{\text{Alfven}} = \pm 3^\circ$ can still be related to the MAW. For larger downtail separations, the flux tubes crossed are connected to Ganymede's auroral tail.

### 3. Results

#### 3.1. Ganymede-Magnetosphere Interaction Signatures in JADE and UVS Data

Figures 1 and 2 show the JADE and UVS data obtained during PJ16N and PJ37S, respectively. During these flux tube crossings, the $\Delta\lambda_{\text{Alfven}}$ separations are -14.8° and 15.5°, suggesting a TEB and a tail crossing, respectively. The observations made during the other events studied, not shown in Figures 1 and 2, are displayed in the Supporting Information S1. Table 1 also summarizes the times, positions, and electron properties of all 11 events.

Figures 1a and 2a show the auroral structures observed by UVS during PJ16N and PJ37S, as well as Juno's magnetic footpath projected onto Jupiter's atmosphere, shown as red lines and dots. During the time ranges represented, Juno crossed magnetic field lines with increasing M-Shell values. As a result, the spacecraft first crossed the footpath of Io (PJ16N ~ 19:46, not shown for PJ37S), followed by the one of Europa (PJ16N ~ 20:09, not shown for PJ37S), and the one of Ganymede (PJ16N ~ 20:15, PJ37S ~ 18:19). Finally, Juno crossed the main oval emission region few minutes after it crossed the footpath of Ganymede. The measurements represented in Figures 1b-1d and 2b-2d are obtained close to the estimated time of the crossings of Ganymede's footpath. The crossings of the main oval are identified as large increases of the *EF*, $E_{\text{char}}$, and auroral brightness (Allegrini, Mauk, et al., 2020; Clark et al., 2018; Mauk et al., 2017). Few minutes before the crossings of the main oval, a sudden increase by a factor of ~10 in the electron differential number flux is observed, at a time close to the one estimated by JRM33 + CON2020 for each crossing, that we identify as a signature of the Ganymede-magnetosphere interaction. This conclusion is reinforced by the M-Shell values crossed by Juno at the time of the observations, that is, 15.5 and 15.9 for PJ16N and PJ37S, respectively. These values fall within the M-Shell range covered by Ganymede, from 15 to 17, because of the tilt between the magnetic equator and the orbital plane of the satellites. We note that for the 11 events reported, the median time deviation between the JRM33 + CON2020 estimates of the flux tubes crossings and the actual start of the beginning of the crossings as observed in the JADE data is 13 s. This value, due to magnetic field model and mapping uncertainties, is close to the 14 s median deviation derived by Rabia et al. (2024) who compared the JRM33 + CON2020 estimates with crossings of Io, Europa, and Ganymede flux tubes with in situ observations reported in several publications. In this study, we add 9 potential observations of Ganymede's flux tubes crossings not considered in Rabia et al. (2024), reinforcing the conclusion that JRM33 + CON2020 is accurate in predicting the crossings of moons' magnetic flux tubes.

The signatures of the Ganymede-magnetosphere interactions appear as sudden increases of the electron differential flux, with a typical duration of few tens of seconds (Figures 1b and 2b). This duration strongly depends on the configuration of the flux tube crossing. When simultaneous coverage of the upward and downward LC is available, the observed electron beams are always bidirectional in the pitch angle domain (Figures 1c and 2c), which is consistent with the previous observations of the Io- and Europa-magnetosphere interactions (Allegrini, Gladstone, et al., 2020; Hue et al., 2022; Rabia et al., 2023; Szalay et al., 2018, 2020b). This feature, predicted by theoretical (Hess et al., 2010) and modeling (Damiano et al., 2019) works, suggests an acceleration by inertial Alfvén waves. The observation of both downward and upward filled loss cones also suggests that Juno lies within the acceleration region. Indeed, only the downward LC is expected to be filled if Juno is below the acceleration region, and that only the upward one if Juno is above this region. The altitude range sampled during the
<figure><img src="image_4.png" /><figcaption>**Figure 1.** JADE in situ and UVS remote observations made during PJ16N. (a) UV false color image of the auroral emissions observed close to Ganymede's footprint. The Juno footpath and the instantaneous footprints of the Galilean moons derived using the JRM33 + CON2020 models are shown as red lines and orange dots, respectively. The boundary of the time window over which the UVS data has been co-added is shown at the bottom right corner, and is reported on the Juno footpath as two red dots. The white triangles and crosses along the Juno footpath highlight Juno's instantaneous footprints with a 10 and 2 min time step, respectively. (b) Electron differential number flux measured by JADE-E. The *EF* is superimposed. (c) Pitch angle distribution. The size of the loss cones at the time of the flux tube crossing is indicated by the dashed line. (d) Arbitrary brightness related to the number of UVS total countrate, UVS false color along the footpath of Juno and electron characteristic energy. The information related to the position of Juno are indicated below the panel (d). The times for the flux tubes crossings estimated from JRM33 + CON2020 are represented by vertical gray lines in panels (b–d). Events associated with a Ganymede's flux tube crossing are highlighted by an orange rectangle while the crossing of the main oval is displayed, in panels (b, c, d), as a purple rectangle.</figcaption></figure>

<figure><img src="image_5.png" /><figcaption>**Figure 2.** Same as Figure 1, for PJ37S.</figcaption></figure>
<table><caption>**Table 1**

Times and Positions for Which We Identified Ganymede-Magnetosphere Interaction Signatures in the JADE-E and UVS Data</caption><thead><tr><th>PJ<br>& Hem</th><th>Date</th><th>T<sub>start</sub></th><th>T<sub>stop</sub></th><th>T<sub>predicted</sub></th><th>Δλ<sub>Alfvén</sub><br>[°]</th><th>Juno<br>alt [R<sub>J</sub>]</th><th>Gan.<br>θ<sub>mag</sub> [°]</th><th>EF<br>[mW/m<sup>2</sup>]</th><th>E<sub>char</sub><br>[keV]</th><th>Interaction region<br>size [R<sub>Gan</sub>]</th><th>UVS integration<br>time [s]</th><th>UVS-JADE<br>shift [s]</th></tr></thead><tbody><tr><td>16N</td><td>2018-10-29</td><td>20:15:06</td><td>20:15:09</td><td>20:15:28</td><td>-14.83</td><td>0.980</td><td>-8.86</td><td>63.88</td><td>29.46</td><td>2.112</td><td>331</td><td>5</td></tr><tr><td>30S</td><td>2020-11-08</td><td>02:55:00</td><td>02:55:03</td><td>02:54:58</td><td>-6.30</td><td>1.325</td><td>1.82</td><td>280.0</td><td>18.034</td><td>2.435</td><td>572</td><td>10</td></tr><tr><td>20N</td><td>2019-05-29</td><td>07:37:19</td><td>07:37:31</td><td>07:37:36</td><td>0.57</td><td>0.540</td><td>-8.35</td><td>15.524</td><td>3.459</td><td>26.598</td><td>457</td><td>-3</td></tr><tr><td>17S</td><td>2018-12-21</td><td>18:03:40</td><td>18:03:58</td><td>18:03:06</td><td>4.47</td><td>1.279</td><td>6.94</td><td>13.539</td><td>1.5</td><td>16.999</td><td>1,548</td><td>30</td></tr><tr><td>37S</td><td>2021-10-16</td><td>18:19:18</td><td>18:20:07</td><td>18:18:48</td><td>15.48</td><td>1.322</td><td>8.06</td><td>7.0869</td><td>1.811</td><td>22.543</td><td>333</td><td>-35</td></tr><tr><td>21N</td><td>2019-07-21</td><td>03:05:24</td><td>03:05:34</td><td>03:05:14</td><td>16.89</td><td>1.144</td><td>-1.38</td><td>6.349</td><td>3.407</td><td>8.434</td><td>452</td><td>20</td></tr><tr><td>4N</td><td>2017-02-02</td><td>12:26:23</td><td>12:26:29</td><td>12:26:36</td><td>26.85</td><td>0.516</td><td>-5.99</td><td>16.684</td><td>0.942</td><td>17.997</td><td>638</td><td>5</td></tr><tr><td>22S</td><td>2019-09-12</td><td>04:30:18</td><td>04:30:31</td><td>04:30:22</td><td>41.35</td><td>0.949</td><td>-7.57</td><td>6.553</td><td>2.091</td><td>15.611</td><td>632</td><td>35</td></tr><tr><td>14S</td><td>2018-07-16</td><td>06:07:30</td><td>06:07:57</td><td>06:07:30</td><td>45.79</td><td>0.954</td><td>10.11</td><td>5.88</td><td>1.978</td><td>20.944</td><td>992</td><td>5</td></tr><tr><td>41N</td><td>2022-04-09</td><td>14:59:18</td><td>14:59:59</td><td>15:00:22</td><td>51.05</td><td>0.930</td><td>-2.85</td><td>5.967</td><td>3.143</td><td>16.243</td><td>1,160</td><td>-10</td></tr><tr><td>27S</td><td>2020-06-02</td><td>11:10:13</td><td>11:10:31</td><td>11:10:00</td><td>51.77</td><td>0.950</td><td>-0.45</td><td>4.19</td><td>1.466</td><td>21.014</td><td>1,053</td><td>-50</td></tr></tbody></table>

Note. Electrons properties derived, displayed in Figures 1–3 are reported.

observations reported, that is, 0.5–1.3 $R_J$ (Figure 3, Table 1) could therefore be an indication of the altitude of the acceleration region.

During PJ16N, identified as a TEB crossing, the electron characteristic energy $E_{char}$ raises up to ~30 keV while during PJ37S, identified as a tail crossing, this increase is smaller, around 2 keV. These values are representative of the other events studied, with a significantly higher $E_{char}$ in the TEB compared to the one in the MAW and tail (Table 1, Figure 3c).

Figures 1d and 2d show the brightness and the false color UV emissions observed along the Juno footpath during PJ16N and PJ37S, respectively. For both events, we note a small time offset between the JADE and UVS measurements. Indeed, taking the PJ37S observations as an example, the crossing of the main oval is observed in the JADE-E measurements at around 18:22:30 while it appears in the UVS data as a brighter emission along Juno's footpath at around 18:23:30. Similar time offsets were also observed by Allegrini, Mauk, et al. (2020) and Al Saati et al. (2022) who studied the crossings of the main auroral oval during the first 9 and 30 perijoves, respectively. This may result from (a) uncertainties on the projections of the Juno magnetic footprint or the auroral emissions onto Jupiter's poles, independent from the magnetic mapping uncertainties (b) temporal differences due to the fact that UVS observations are not truly simultaneous with JADE and instead results from integrating over a certain temporal range as close as possible from the JADE measurement window, and/or (c) projection effects resulting from UVS observing extended auroral structures smeared over several co-added Juno spins with different vantage points. We quantify the JADE-UVS temporal offset by comparing their observations of the main oval crossings for all the events studied. We note that this quantification is only an estimate of the JADE-UVS temporal offset since it remains challenging to identify precisely the start of the main auroral oval crossing in both data set (Allegrini, Mauk, et al., 2020). The values derived are provided in Table 1. They correspond to the times we applied to the UVS data to match the JADE-E in situ measurements.
<figure><img src="image_6.png" /><figcaption>**Figure 3.** (a) Projection of Juno position onto Ganymede's orbital plane at the times of flux tubes crossings. Ganymede orbital distance is indicated with a gray dotted line. (b) Precipitating *EF*. The exponential decay law that best fits the data set is shown. Horizontal black lines represent the width of the bins used to bin the energy flux values. (c) Characteristic electron energy. (d) Size of the interaction region projected onto Ganymede orbital plane and estimated from the duration of the acceleration events. The color code used refers to the altitude of the crossing while the markers indicate the hemisphere in which the flux tube crossing was observed. At the top of the figure, we indicate the auroral structure created by the electrons within the crossed flux tubes, estimated with the $\Delta\lambda_{Alfvén}$ separation.</figcaption></figure>

## 3.2. Statistical Study

In order to confirm that the observations are related to a Ganymede's flux tube crossing by Juno, we project the spacecraft position at the time of the crossing onto the moon's orbital plane. The results, presented in Figure 3a, show that all the signatures observed in the JADE-E data map between $R = 14.3 R_⊕$ and $R = 16.3 R_⊕$, which is close to Ganymede's orbital distance, that is, $R = 14.95 \pm 0.02 R_⊕$. Deviations from Ganymede's semi-major axis may result from (a) magnetic field mapping uncertainties or (b) a non-strictly azimuthal translation of the disturbances in the wake of Ganymede, which modified the radial distance location of the electron beams source.

Figure 3b shows the maximum precipitating *EF*, that is, the *EF* within the downward LC, measured during each of the flux tubes crossings identified as a function of the $\Delta\lambda_{Alfvén}$ separation. We also bin the *EF* values in 15° intervals and perform an exponential fit, excluding the *EF* measured in the TEB. We find that the *EF* decreases with downtail distance. In Figure 3b, we show the decay profile that minimizes the root mean square error (RMSE = 0.235). We find that the e-folding value of ~29°, which quantifies the *EF* decrease with the downtail distance, better matches our limited data set. This is consistent with the e-folding value of 24° derived by Bonfond, Saur, et al. (2017) that fit the decrease of the Ganymede's auroral tail UV brightness using HST observations. The fit presented in Figure 3c, which also minimize the RMSE (RMSE = 0.852), shows that the correlation between $E_{char}$ and $\Delta\lambda_{Alfvén}$ is very weak, meaning that $E_{char}$ is nearly constant in the MAW and auroral tail flux tube.

In Figure 3d, we estimate the size of the interaction region in the equatorial plane in these three regions. To do so, we project Juno's position at the start and end of the flux tubes crossings onto Ganymede's orbital plane. Error bars are derived assuming a $\pm 1$ s uncertainty on the start and end of the flux tubes crossing as observed in JADE-E data. We observe a large discrepancy between the size of the interaction region derived in the TEB, MAW, and auroral tail. Using the two crossings of the TEB, we derive a mean size for the interaction region of $2.3 \pm 1.5$
<figure><img src="image_7.png" /><figcaption>**Figure 4.** Electron energy distribution within the downward LC observed within flux tubes connected to the TEB spot (a), MAW spot (b) and auroral tail (c). Colored curves show the distribution every second measured within the flux tubes. Gray curves represent the distribution measured in 15-s intervals before and after the flux tube crossing. Gray areas indicate the energy range not covered by the JADE-E instrument as a result of a change of in instrument operation after PJ32.</figcaption></figure>

$R_{\text{Gan}}$, where $1 R_{\text{Gan}} = 2,634$ km. The size obtained using the MAW crossing, that is, ~26.5 ± 4.4 $R_{\text{Gan}}$, is the largest. Finally, in the tail, the mean size derived by averaging 8 observations at various $\Delta\lambda_{\text{Alfvén}}$ separations is ~17.5 ± 2.2 $R_{\text{Gan}}$. With our limited data set, we do not find any correlation between the interaction size and $\Delta\lambda_{\text{Alfvén}}$ separation as reported for Io (Szalay et al., 2020b) but rather a constant value as reported for Europa (Rabia et al., 2023).

### 3.3. Energy Distribution

We have shown that Juno sampled electrons within Ganymede's TEB, MAW, and auroral tail. Here, we investigate their properties in these different regions, in particular their energy spectra. Figure 4 shows the electron energy distribution, that is, the electron DNF within the downward LC as a function of energy, for PJ16N, PJ20N, and PJ37S which are identified as crossings of flux tubes connected to the TEB, MAW and auroral tail, respectively. The electron spectra for the other events studied, not presented here, are provided in Figure S6 in Supporting Information S1.

It appears that in the TEB (Figure 4a), the electrons exhibit non-monotonic spectra, with a clear increase of the DNF at a specific energy which correspond roughly to $E_{\text{char}}$. At others energies, the DNF is similar to the magnetospheric background flux. The other Ganymede's TEB crossing observation, reported by Hue et al. (2022) presented a similar behavior, with a DNF increase for electrons in the 2–35 keV range. We note that the electrons in Europa's TEB identified by Rabia et al. (2023) also exhibit a non-monotonic spectra, albeit with a lower $E_{\text{char}}$.

In the MAW and tail, the electron energy distributions take the form of broadband spectra (Figures 4b and 4c). The electron DNF increase is observed over a wide energy range, that is, for $E > 1$ keV in the MAW (Figure 4b) and $E > 0.1$ keV in the auroral tail (Figure 4c). This means that electrons are accelerated at all the corresponding energies. This type of distribution has been systematically observed in flux tubes connected to Io, Europa, and Ganymede MAW and auroral tails (Rabia et al., 2023; Szalay et al., 2020a, 2020b).

### 4. Discussion

Using a cross-correlation between magnetic field line mapping, JADE, and UVS data, we identified 11 events during which Juno crossed the magnetic shell of Ganymede. For these events, Juno observed bidirectional electrons beams (Figures 1c and 2c), with a characteristic energy between 1 and 30 keV (Figure 3c). These measurements suggest that Juno transited within the acceleration region, at an altitude between 0.5 and $1.3 R_{\text{J}}$.

We organized the observations as a function of the $\Delta\lambda_{\text{Alfvén}}$ separation, a metric that takes into account the propagation of Alfvén waves from moons' orbits to Jupiter's atmosphere based on HST or Juno-UVS observations (Hue et al., 2023), as previously done for Io and Europa studies (Rabia et al., 2023; Szalay et al., 2020b). We show that for Ganymede the $\Delta\lambda_{\text{Alfvén}}$ metric is also the most appropriate one to organize the EF as a function of downtail distance (Figure 3b). This does not rule out that a dependence with Ganymede's magnetic and centrifugal latitudes
could exist too since it is expected that Ganymede encounters a denser plasma flow when the moon lies within the magnetodisc. Such a dependency may however be difficult to identify since the time variability of the magnetospheric conditions also plays a role in the strength of the moon-magnetosphere interactions. In contrast, there is no clear correlation between $E_{char}$ and the $\Delta\lambda_{Alfven}$ separation, $E_{char}$ being almost constant in the MAW and auroral tail, with a mean value of 2.2 keV.

Following the observation of a correlation between the precipitating EF and the $\Delta\lambda_{Alfven}$ separation, we constrain an e-folding value of 29° for the in situ measurements (Figure 3b), consistent with 24° derived from fitting the brightness decay of Ganymede's auroral tail using HST observations (Bonfond, Saur, et al., 2017). We note that previous statistical studies on Io and Europa derived EF e-folding values of 21° and 7°, respectively (Rabia et al., 2023; Szalay et al., 2020b). It is surprising that the e-folding value of electron EF at Ganymede is slightly higher than the one of Io as the extent of Io's auroral tail extent is larger than that of Ganymede. A greater number of Ganymede flux tube crossings would help to better constrain the EF e-folding.

We found a clear distinction between the properties of the electrons creating the TEB spot and those measured in the MAW, and auroral tail flux tubes. Indeed, it appears that electrons measured within the flux tubes connected to Ganymede's TEB spot ($\Delta\lambda_{Alfven} < -3°$) exhibit a significantly higher downward EF and $E_{char}$ (Figures 3b and 3c). In Europa's TEB flux tubes, higher EF and $E_{char}$ were also reported (Rabia et al., 2023). At Io, an observation of a large EF of ~600 mW/m² has been reported by Szalay et al. (2020b) but the positive $\Delta\lambda_{Alfven}$ separation during this event was not consistent with a TEB crossing which was therefore attributed to a MAW crossing.

We estimated the size of the interaction region in Ganymede's orbital plane by mapping magnetically the position of Juno during the crossings. We found a clear distinction between the estimates based on TEB crossings and those derived from crossings of flux tubes connected to the auroral tail. By expressing the size estimated using TEB crossings in kilometers and comparing to the one reported at Europa (Allegrini, Gladstone, et al., 2020; Allegrini, Mauk, et al., 2020; Rabia et al., 2023), we found a size of ~6,000 km for both moons. These similar observations, made on two moons of very different sizes, may suggest that the size of the interaction region derived using TEB crossings are independent of the size of the obstacle, that is, the moons, but are rather an indication of the width of the flux tubes where the electron are accelerated in the upward direction. However, the low number of TEB crossing observations does not allow us to draw firm conclusion about the origin of this smaller interaction size derived. The size derived using the MAW crossing during PJ20N, that is, $26.5 \pm 4.4 R_{Gan}$, is slightly higher than the estimate of $8-20 R_{Gan}$ estimated from the size of the MAW spot observed by HST (Grodent et al., 2009). In the tail, we estimated the size of the interaction region to be $17.5 \pm 2.2 R_{Gan}$, which is ~3-4 times larger than the estimates at Io and Europa ($5.6 R_{Io}$ and $4.2 R_{Eur}$). We note that estimates of the interaction region size larger than the size of the moons have been also reported at Io and Europa (Rabia et al., 2023; Szalay et al., 2020b). However, this must be compared with the size of the obstacle offered to the magnetospheric plasma flow by these three objects. Considering that Io interacts with the extent of its ionosphere (~$2.8 R_{Io}$, Saur, 2021), Europa only with its small exosphere (~$2 R_{Eur}$) and Ganymede with its magnetosphere (~$6 R_{Gan}$, Jia et al., 2009; Jia & Kivelson, 2021), a correlation between the size of the obstacle $R_{obstacle}$ and the size of the interaction region in moons' wake derived with flux tubes crossings $R_{wake}$ can be established. Based on the values reported at Io and Europa by Szalay et al. (2020b) and Rabia et al. (2023), we find that $(R_{wake}/R_{obstacle}) = 2$ at Io, $(R_{wake}/R_{obstacle}) = 2.1$ at Europa and $(R_{wake}/R_{obstacle}) = 2.9$ at Ganymede. These observations, which do not reflect the results of MHD simulations of the local environment of the moons, require investigation by future studies considering the propagation of the disturbances in far-field regions.

These two different regimes are also found when looking at the electron energy distributions. In the MAW and auroral tail, the electron distributions are always observed to be broadband. These broadband distributions could be explained by acceleration processes involving inertial Alfvén waves (Damiano et al., 2019). Evidence for Alfvénic acceleration in the flux tubes of Ganymede has also been raised by Louis et al. (2020, 2023) and Mauduit et al. (2023) who use a diagnostic of the Ganymede-induced radio emission. Since the TEB is formed by an anti-planetward acceleration from the MAW (Bonfond et al., 2008), we expect to observe the same distribution for electrons creating the MAW and TEB spots. However, we have shown that in the TEB, electrons exhibit a non-monotonic distribution with a DNF increase at a specific energy close to $E_{char}$ (Figure 4a). We suggest that only a part of an initial broadband energy distribution resulting from an anti-planetward acceleration reaches the opposite hemisphere. During the propagation from the acceleration region toward the opposite hemisphere, most
of the energy distribution might be scattered and/or undergoes additional wave-particle interactions occurring
during the crossing of the magnetodisc, preventing them to propagate all the way down to the auroral regions. The
energy distribution measured in the TEB flux tube, which only contains the particles that propagate all the way, is
therefore different from the initial broadband distribution.

Since we only reported in the present paper observations of electrons within the downward loss cone, additional
studies are required to confirm that the electron energy distribution in the upward loss cone is also broadband and
compatible with an acceleration process involving Alfvén waves. Moreover, measurements during a crossing of
Io's TEB, still unreported, could provide new insights into the origin of the TEB in moon-magnetosphere
interactions.

5. Conclusions

We characterized the properties of electrons accelerated by the Ganymede-magnetosphere interactions using a
joint analysis of Juno in situ plasma and remote UV auroral measurements. The main outcomes of our statistical
analysis are as follows:

1. The combination of JADE-E measurements and UVS observations with field line tracing enables us to identify 11 events when Juno can diagnose in situ the properties of electrons accelerated by the Ganymede—Jovian magnetosphere interaction.

2. We find a clear dependency of *EF* with the $\Delta\lambda_{\text{Alfvén}}$ separation. The e-folding value from our in situ observations, that is, 29°, is consistent with the value of 24°, previously derived with HST observations.

3. The properties of electrons measured in flux tubes connected to the TEB spot, that is, *EF*, *E*<sub>char</sub> and energy distribution, are significantly different than those creating the MAW spot and the auroral tail. Further theoretical and modeling studies on acceleration processes are required to explain these differences.

4. The size of the interaction region in Ganymede's orbital plane is estimated to be $17.5 \pm 2.2 R_{\text{Gan}}$, based on the measurements made within the flux tubes connected to the auroral tail.

5. The observation of bidirectional electron beams suggests that Juno was located within the acceleration region during these measurements. Thus, we estimate that this one is located between an altitude of 0.5 $R_J$ to 1.3 $R_J$ at least.

Data Availability Statement

JADE (Allegrini, 2023) and UVS data (Trantham, 2014) used in this study are publicly available on the Planetary Data System, nodes Planetary Plasma Interactions and Planetary Atmospheres, respectively. Part of the analysis have been done using the CLWEB software (http://clweb.irap.omp.eu) developed by E. Penou at IRAP and the AMDA software (https://amda.cdpp.eu) provided by CDPP (http://www.cdpp.eu/).

Acknowledgments

French co-authors acknowledge the support of CNES to the Juno mission. This study has been partially supported through the Grant EUR TESS No. ANR-18-EURE-0018 in the framework of the Programme des Investissements d'Avenir. The research performed by N.A. and Q.N. holds as part of the project FACOM (ANR-22-CE49-0005-01 ACT) and has benefited from a funding provided by l'Agence Nationale de la Recherche (ANR) under the Generic Call for Proposals 2022. The work at SwRI was funded by the NASA New Frontiers Program for Juno through contract NNM06AA75C. V.H. acknowledges support from the French government under the France 2030 investment plan, as part of the Initiative d'Excellence d'Aix-Marseille Université —A*MIDEX AMX-22-CPJ-04.

References

Acuña, M. H., Neubauer, F. M., & Ness, N. F. (1981). Standing Alfvén wave current system at Io: Voyager 1 observations. *Journal of Geophysical Research*, *86*(A10), 8513–8521. https://doi.org/10.1029/JA086iA10p0851

Allegrini, F. (2023). JNO-J/SW-JAD-5-CALIBRATED-V1.0 [Dataset]. NASA. https://doi.org/10.17189/2775-4623

Allegrini, F., Gladstone, G. R., Hue, V., Clark, G., Szalay, J. R., Kurth, W. S., et al. (2020). First report of electron measurements during a Europa footprint tail crossing by Juno. *Geophysical Research Letters*, *47*(18), e2020GL089732. https://doi.org/10.1029/2020GL089732

Allegrini, F., Mauk, B. H., Clark, G., Gladstone, G. R., Hue, V., Kurth, W. S., et al. (2020). Energy flux and characteristic energy of electrons over Jupiter's main auroral emission. *Journal of Geophysical Research: Space Physics*, 125(4), e2019JA027693. https://doi.org/10.1029/2019JA027693

Al Saati, S., Clément, N., Louis, C., Blanc, M., Wang, Y., André, N., et al. (2022). Magnetosphere-ionosphere-thermosphere coupling study at Jupiter based on Juno's first 30 orbits and modeling tools. *Journal of Geophysical Research: Space Physics*, 127(10), e2022JA030586. https://doi.org/10.1029/2022JA030586

Bolton, S., Lunine, J., Stevenson, D., Connerney, J., Levin, S., Owen, T., et al. (2017). The Juno mission. *Space Science Reviews*, 213(1), 5–37. https://doi.org/10.1007/s11214-017-0429-6

Bonfond, B., Gladstone, G. R., Grodent, D., Greathouse, T. K., Versteeg, M. H., Hue, V., et al. (2017). Morphology of the UV aurorae Jupiter during Juno's first perijove observations. *Geophysical Research Letters*, 44(10), 4463–4471. https://doi.org/10.1002/2017GL073114

Bonfond, B., Grodent, D., Gérard, J.-C., Radioti, A., Dols, V., Delamere, P. A., & Clarke, J. T. (2009). The Io UV footprint: Location, inter-spot distances and tail vertical extent. *Journal of Geophysical Research*, 114(A7), A07224. https://doi.org/10.1029/2009JA014312

Bonfond, B., Grodent, D., Gérard, J.-C., Radioti, A., Saur, J., & Jacobsen, S. (2008). UV Io footprint leading spot: A key feature for understanding the UV Io footprint multiplicity? *Geophysical Research Letters*, 35(5), L05107. https://doi.org/10.1029/2007GL032418

Bonfond, B., Saur, J., Grodent, D., Badman, S., Bisikalo, D., Shematovich, V., et al. (2017). The tails of the satellite auroral footprints at Jupiter. *Journal of Geophysical Research: Space Physics*, 122(8), 7985–7996. https://doi.org/10.1002/2017ja024370
Clark, G., Mauk, B. H., Kollmann, P., Szalay, J. R., Sulaiman, A. H., Gershman, D. J., et al. (2020). Energetic proton acceleration associated with Io's footprint tail. *Geophysical Research Letters*, 47(24), e2020GL090839. https://doi.org/10.1029/2020GL090839

Clark, G., Tao, C., Mauk, B. H., Nichols, J., Saur, J., Bunce, E. J., et al. (2018). Precipitating electron energy flux and characteristic energies in Jupiter's main auroral region as measured by Juno/JEDI. *Journal of Geophysical Research: Space Physics*, 123(9), 7554–7567. https://doi.org/10.1029/2018JA025639

Clarke, J. T., Ajello, J., Ballester, G., Ben Jaffel, L., Connerney, J., Gérard, J.-C., et al. (2002). Ultraviolet emissions from the magnetic footprints of Io, Ganymede and Europa on Jupiter. *Nature*, 415(6875), 997–1000. https://doi.org/10.1038/415997a

Clarke, J. T., Ballester, G., Trauger, J., Ajello, J., Pryor, W., Tobiska, K., et al. (1998). Hubble Space Telescope imaging of Jupiter's UV aurora during the Galileo orbiter mission. *Journal of Geophysical Research*, 103(E9), 20217–20236. https://doi.org/10.1029/98JE01130

Coffin, D., Damiano, P., Delamere, P., Johnson, J., & Ng, C.-S. (2022). Broadband energization of superthermal electrons in Jupiter's inner magnetosphere. *Journal of Geophysical Research: Space Physics*, 127(8), e2022JA030528. https://doi.org/10.1029/2022JA030528

Connerney, J., Benn, M., Bjarno, J., Denver, T., Espley, J., Jorgensen, J., et al. (2017). The Juno magnetic field investigation. *Space Science Reviews*, 213(1–4), 39–138. https://doi.org/10.1007/s11214-017-0334-z

Connerney, J. E. P., Baron, R., Satoh, T., & Owen, T. (1993). Images of excited H+ at the foot of the Io flux tube in Jupiter's atmosphere. *Science*, 262(5136), 1035–1038. https://doi.org/10.1126/science.262.5136.1035

Connerney, J. E. P., Timmins, S., Herceg, M., & Joergensen, J. (2020). A Jovian magnetodisc model for the Juno era. *Journal of Geophysical Research: Space Physics*, 125(10), e2020JA028138. https://doi.org/10.1029/2020ja028138

Connerney, J. E. P., Timmins, S., Oliversen, R. J., Espley, J. R., Joergensen, J. L., Kotsiaros, S., et al. (2022). A new model of Jupiter's magnetic field at the completion of Juno's prime mission. *Journal of Geophysical Research: Planets*, 127(2), e2021JE007055. https://doi.org/10.1029/2021JE007055

Damiano, P. A., Delamere, P. A., Kim, E.-H., Johnson, J. R., & Ng, C. S. (2023). Electron energization by inertial Alfvén waves in density depleted flux tubes at Jupiter. *Geophysical Research Letters*, 50(5), e2022GL102467. https://doi.org/10.1029/2022GL102467

Damiano, P. A., Delamere, P. A., Stauffer, B., Ng, C.-S., & Johnson, J. R. (2019). Kinetic simulations of electron acceleration by dispersive scale Alfvén waves in Jupiter's magnetosphere. *Geophysical Research Letters*, 46(6), 3043–3051. https://doi.org/10.1029/2018GL081219

Gérard, J.-C., Mura, A., Bonfond, B., Gladstone, G., Adriani, A., Hue, V., et al. (2018). Concurrent ultraviolet and infrared observations of the north Jovian aurora during Juno's first perijove. *Icarus*, 312, 145–156. https://doi.org/10.1016/j.icarus.2018.04.020

Gérard, J.-C., Saglam, A., Grodent, D., & Clarke, J. T. (2006). Morphology of the ultraviolet Io footprint emission and its control by Io's location. *Journal of Geophysical Research*, 111(A4), A04202. https://doi.org/10.1029/2005JA011327

Gladstone, G. R., Persyn, S. C., Eterno, J. S., Walther, B. C., Slater, D. C., Davis, M. W., et al. (2017). The ultraviolet spectrograph on NASA's Juno mission. *Space Science Reviews*, 213(1–4), 447–473. https://doi.org/10.1007/s11214-014-0040-z

Goertz, C. (1980). Io's interaction with the plasma torus. *Journal of Geophysical Research*, 85(A6), 2949–2956. https://doi.org/10.1029/JA085iA06p02949

Goldreich, P., & Lynden-Bell, D. (1969). Io, a Jovian unipolar inductor. *The Astrophysical Journal*, 156, 59–78. https://doi.org/10.1086/149947

Greathouse, T., Gladstone, R., Versteeg, M., Hue, V., Kammer, J., Giles, R., et al. (2021). Local time dependence of Jupiter's polar auroral emissions observed by Juno UVS. *Journal of Geophysical Research: Planets*, 126(12), e2021JE006954. https://doi.org/10.1029/2021JE006954

Grodent, D., Bonfond, B., Radioti, A., Gérard, J.-C., Jia, X., Nichols, J. D., & Clarke, J. T. (2009). Auroral footprint of Ganymede. *Journal of Geophysical Research*, 114(A7). https://doi.org/10.1029/2009JA014289

Gurnett, D. A., & Goertz, C. K. (1981). Multiple Alfvén wave reflections excited by Io: Origin of the Jovian decametric arcs. *Journal of Geophysical Research*, 86(A2), 717–722. https://doi.org/10.1029/JA086iA02p00717

Hess, S., Delamere, P., Dols, V., Bonfond, B., & Swift, D. (2010). Power transmission and particle acceleration along the Io flux tube. *Journal of Geophysical Research*, 115(A6), A06205. https://doi.org/10.1029/2009JA014928

Hue, V., Gladstone, G. R., Louis, C. K., Greathouse, T. K., Bonfond, B., Szalay, J. R., et al. (2023). The Io, Europa, and Ganymede auroral footprints at Jupiter in the ultraviolet: Positions and equatorial lead angles. *Journal of Geophysical Research: Space Physics*, 128(5), e2023JA031363. https://doi.org/10.1029/2023JA031363

Hue, V., Greathouse, T. K., Bonfond, B., Saur, J., Gladstone, G. R., Roth, L., et al. (2019). Juno-UVS observation of the Io footprint during solar eclipse. *Journal of Geophysical Research: Space Physics*, 124(7), 5184–5199. https://doi.org/10.1029/2018JA026431

Hue, V., Szalay, J. R., Greathouse, T. K., Bonfond, B., Kotsiaros, S., Louis, C. K., et al. (2022). A comprehensive set of Juno in situ and remote sensing observations of the Ganymede auroral footprint. *Geophysical Research Letters*, 49(7), e2021GL096994. https://doi.org/10.1029/2021GL096994

Jacobsen, S., Neubauer, F. M., Saur, J., & Schilling, N. (2007). Io's nonlinear MHD-wave field in the heterogeneous Jovian magnetosphere. *Geophysical Research Letters*, 34(10), L10202. https://doi.org/10.1029/2006GL029187

Jia, X., & Kivelson, M. G. (2021). The magnetosphere of Ganymede. *Magnetospheres in the solar system*, 557–573. https://doi.org/10.1002/9781119815624.ch35

Jia, X., Walker, R. J., Kivelson, M. G., Khurana, K. K., & Linker, J. A. (2009). Properties of Ganymede's magnetosphere inferred from improved three-dimensional MHD simulations. *Journal of Geophysical Research*, 114(A9), A09209. https://doi.org/10.1029/2009JA014375

Louis, C. K., Louarn, P., Allegrini, F., Kurth, W. S., & Szalay, J. R. (2020). Ganymede-induced decametric radio emission: In situ observations and measurements by Juno. *Geophysical Research Letters*, 47(20), e2020GL090021. https://doi.org/10.1029/2020GL090021

Louis, C. K., Louarn, P., Collet, B., Clément, N., Al Saati, S., Szalay, J. R., et al. (2023). Source of radio emissions induced by the Galilean Moons Io, Europa and Ganymede: In situ measurements by Juno. *Journal of Geophysical Research: Space Physics*, 128(12), e2023JA031985. https://doi.org/10.1029/2023JA031985

Lysak, R. L., Sulaiman, A. H., Bagenal, F., & Crary, F. (2023). A numerical model for the interaction of Io-generated Alfvén waves with Jupiter's magnetosphere and ionosphere. *Journal of Geophysical Research: Space Physics*, 128(4), e2022JA031180. https://doi.org/10.1029/2022JA031180

Mauduit, E., Zarka, P., Lamy, L., & Hess, S. L. (2023). Drifting discrete Jovian radio bursts reveal acceleration processes related to Ganymede and the main aurora. *Nature Communications*, 14(1), 5981. https://doi.org/10.1038/s41467-023-41617-8

Mauk, B. H., Clarke, J., Grodent, D., Waite Jr, J., Paranicas, C., & Williams, D. (2002). Transient aurora on Jupiter from injections of magnetospheric electrons. *Nature*, 415(6875), 1003–1005. https://doi.org/10.1038/4151003a

Mauk, B. H., Haggerty, D. K., Paranicas, C., Clark, G., Kollmann, P., Rymer, A. M., et al. (2017). Juno observations of energetic charged particles over Jupiter's Polar Regions: Analysis of monodirectional and bidirectional electron beams. *Geophysical Research Letters*, 44(10), 4410–4418. https://doi.org/10.1002/2016GL072286
McComas, D., Alexander, N., Allegrini, F., Bagenal, F., Beebe, C., Clark, G., et al. (2017). The Jovian auroral distributions experiment (JADE) on the Juno mission to Jupiter. *Space Science Reviews*, 213(1), 547–643. https://doi.org/10.1007/s11214-013-9990-9

Mura, A., Adriani, A., Altieri, F., Connerney, J. E. P., Bolton, S. J., Moriconi, M. L., et al. (2017). Infrared observations of Jovian aurora from Juno's first orbits: Main oval and satellite footprints. *Geophysical Research Letters*, 44(11), 5308–5316. https://doi.org/10.1002/2017GL072954

Mura, A., Adriani, A., Connerney, J. E. P., Bolton, S. J., Altieri, F., Bagenal, F., et al. (2018). Juno observations of spot structures and a split tail in Io-induced aurorae on Jupiter. *Science*, 361(6404), 774–777. https://doi.org/10.1126/science.aat1450

Neubauer, F. (1980). Nonlinear standing Alfvén wave current system at Io: Theory. *Journal of Geophysical Research: Space Physics*, 85(A3), 1171–1178. https://doi.org/10.1029/JA085iA03p01171

Neubauer, F. (1998). The sub-Alfvénic interaction of the Galilean satellites with the Jovian magnetosphere. *Journal of Geophysical Research*, 103(E9), 19843–19866. https://doi.org/10.1029/97JE03370

Prangé, R., Rego, D., Southwood, D., Zarka, P., Miller, S., & Ip, W. (1996). Rapid energy dissipation and variability of the Io–Jupiter electro- dynamic circuit. *Nature*, 379(6563), 323–325. https://doi.org/10.1038/379323a0

Pryor, W. R., Magalhães, F. P., Lamy, L., Prangé, R., Esposito, L. W., Gustin, J., et al. (2024). Cassini UVIS observations of the Enceladus auroral footprint on Saturn in 2017. *The Planetary Science Journal*, 5(1), 20. https://doi.org/10.3847/PSJ/ad0cbc

Pryor, W. R., Rymer, A. M., Mitchell, D. G., Hill, T. W., Young, D. T., Saur, J., et al. (2011). The auroral footprint of Enceladus on Saturn. *Nature*, 472(7343), 331–333. https://doi.org/10.1038/nature09928

Rabia, J., Hue, V., Szalay, J. R., André, N., Nénon, Q., Blanc, M., et al. (2023). Evidence for non-monotonic and broadband electron distributions in the Europa footprint tail revealed by Juno in situ measurements. *Geophysical Research Letters*, 50(12), e2023GL103131. https://doi.org/10.1029/2023GL103131

Rabia, J., Nénon, Q., André, N., Hue, V., Santos-Costa, D., Kamran, A., & Blanc, M. (2024). Influence of the Jovian current sheet models on the mapping of the UV auroral footprints of Io, Europa, and Ganymede. *Journal of Geophysical Research: Space Physics*, 129(1), https://doi.org/10.1029/2023JA032041

Sarkango, Y., Szalay, J. R., Sulaiman, A. H., Damiano, P. A., McComas, D. J., Rabia, J., et al. (2024). Resonant plasma acceleration at Jupiter driven by satellite-magnetosphere interactions. *Geophysical Research Letters*, 51(5), e2023GL107431. https://doi.org/10.1029/2023GL107431

Saur, J. (2021). Overview of Moon–magnetosphere interactions. In *Magnetospheres in the solar System* (pp. 575–593). American Geophysical Union (AGU). https://doi.org/10.1002/9781119815624.ch36

Saur, J., Janser, S., Schreiner, A., Clark, G., Mauk, B. H., Kollmann, P., et al. (2018). Wave-particle interaction of Alfvén waves in Jupiter's magnetosphere: Auroral and magnetospheric particle acceleration. *Journal of Geophysical Research: Space Physics*, 123(11), 9560–9573. https://doi.org/10.1029/2018JA025948

Sulaiman, A. H., Hospodarsky, G., Elliott, S., Kurth, W., Gurnett, D., Imai, M., et al. (2020). Wave-particle interactions associated with Io's auroral footprint: Evidence of Alfvén, ion cyclotron, and whistler modes. *Geophysical Research Letters*, 47(22), e2020GL088432. https://doi.org/10.1029/2020gl088432

Sulaiman, A. H., Kurth, W. S., Hospodarsky, G. B., Averkamp, T. F., Ye, S.-Y., Menietti, J. D., et al. (2018). Enceladus auroral hiss emissions during Cassini's Grand Finale. *Geophysical Research Letters*, 45(15), 7347–7353. https://doi.org/10.1029/2018GL078130

Sulaiman, A. H., Szalay, J. R., Clark, G., Allegrini, F., Bagenal, F., Brennan, M. J., et al. (2023). Poynting fluxes, field-aligned current densities, and the efficiency of the Io-Jupiter electrodynamic interaction. *Geophysical Research Letters*, 50(10), e2023GL103456. https://doi.org/10.1029/2023GL103456

Szalay, J. R., Allegrini, F., Bagenal, F., Bolton, S. J., Bonfond, B., Clark, G., et al. (2020a). Alfvénic acceleration sustains Ganymede's footprint tail aurora. *Geophysical Research Letters*, 47(3), e2019GL086527. https://doi.org/10.1029/2019GL086527

Szalay, J. R., Allegrini, F., Bagenal, F., Bolton, S. J., Bonfond, B., Clark, G., et al. (2020b). A new framework to explain changes in Io's footprint tail electron fluxes. *Geophysical Research Letters*, 47(18), e2020GL089267. https://doi.org/10.1029/2020GL089267

Szalay, J. R., Bagenal, F., Allegrini, F., Bonfond, B., Clark, G., Connerney, J. E. P., et al. (2020). Proton acceleration by Io's Alfvénic interaction. *Journal of Geophysical Research: Space Physics*, 125(1), e2019JA027314. https://doi.org/10.1029/2019JA027314

Szalay, J. R., Bonfond, B., Allegrini, F., Bagenal, F., Bolton, S., Clark, G., et al. (2018). In situ observations connected to the Io footprint tail Aurora. *Journal of Geophysical Research: Planets*, 123(11), 3061–3077. https://doi.org/10.1029/2018JE005752

Trantham, B. (2014). Juno Jupiter UVS calibrated data archive V1.0 [Dataset]. *PDS Atmospheres (ATM) Node*. https://doi.org/10.17189/c32j-7r56

Yung, Y. L., Gladstone, G. R., Chang, K. M., Ajello, J. M., & Srivastava, S. K. (1982). H2 fluorescence spectrum from 1200 to 1700 A by electron impact—Laboratory study and application to jovian aurora. *The Astrophysical Journal Letters*, 254, L65–L69. https://doi.org/10.1086/183757