MIST
Magnetosphere, Ionosphere and Solar-Terrestrial
Energetic Proton Dropouts During the Juno Flyby of Europa Strongly Depend on Magnetic Field Perturbations
Energetic Proton Dropouts During the Juno Flyby of Europa Strongly Depend on Magnetic Field Perturbations
By Hans Huybrighs (DIAS)
In September 2022 NASA's Juno spacecraft flew by Jupiter's ocean moon Europa. In this study we analyzed energetic ion dropouts measured near Europa. We care about energetic ions because they bombard Europa's icy surface . While they make the surface inhospitable, they might also help produce oxidants from the ice that could form a source of energy for life in the ocean.
The Juno measurements show what happens with the energetic protons at 350 km above the surface, in Europa’s wake (considering the general sense of motion of the protons). There, protons have disappeared, compared to further away where they are abundant. The cartoon below shows some classical ideas about what happens to the protons near Europa (panel 1-2).
Using particle tracing simulations of the ions we can show that the deflections by magnetic fields (3) are also important. In fact, at 100 keV magnetic deflections are the dominant factor that determine the ion abundance. At 1 MeV its a combination of magnetic deflections and the effect shown in panel 2. The simulations also show that the shape of the proton dropout region depends on the exact configuration of the magnetic field, which can vary depending on the atmosphere and electron beams in the wake. All this helps us better understand what happens with the energetic ions and shows us that our ideas of Europa's atmosphere and magnetic fields are reasonable but that improvements can be made.
See publication for details:
, , , , , , et al. (2025). Energetic proton dropouts during the Juno flyby of Europa strongly depend on magnetic field perturbations. Journal of Geophysical Research: Space Physics, 130, e2025JA034000. https://doi.org/10.1029/2025JA034000
Estimating Soft X-Ray Emission from Uranus's Magnetosheath
Estimating Soft X-Ray Emission from Uranus's Magnetosheath
By Dan Naylor (Lancaster University)
Soft X-rays can be generated within planetary magnetosheaths due to charge exchange between neutrals and highly charged solar wind ions such as O^7+. Imaging of the soft X-rays is an emerging technology that aims to provide global and dynamic views of the magnetosheath and cusps, and their response to solar wind driving. The ESA-CAS SMILE mission will soon be launched with a soft X-ray imager (SXI) instrument onboard to investigate the terrestrial magnetosheath. We explore the viability of similar investigations at Uranus.
Uranus has one of the most unusual and complex environments in the solar system. A large obliquity combined with a highly tilted, offset magnetic axis result in an asymmetric and constantly varying magnetosphere where the plasma and neutral source rates from the moons are unconstrained. We impose a simple bullet shaped magnetopause and moon tori informed by Voyager 2 observations to predict soft X-ray emission from the Uranian magnetosheath. We estimate volumetric emission rates of soft X-rays are on the order of 10^-10 photon cm^-3 s^-1, being higher at equinox due to the orientation of the magnetosheath relative to the moon tori. Simple estimates of intensity and flux find that a SMILE-like instrument could detect ~100 photons in a quarter of a planetary rotation at a distance of 212 R_U, as shown in the figure. A hypothetical future imager, with improved FOV and effective area, would detect ~20,000 photons per planetary rotation at 100 R_U. These are promising initial results that suggest imaging of the magnetosheath is possible within key system timescales. Future studies will include magnetospheric cusps and a full range of solar wind ions, which are anticipated to increase emission rates.
Modelled intensity maps for a SMILE‐like SXI at 212 R_U from different viewing geometries at (top row) equinox, where the neutrals are edge-on to the Sun, and (bottom row) solstice, where the neutrals are ring on to the Sun: (a/d) front‐on, (b/e) top‐down and (c/f) side‐on. The different panels show that the amount of flux detected is dependent on viewing position, and an orbital mission should consider the implications of different possible imaging positions.
See publication for details:
Naylor, D., Ray, L. C., Dunn, W. R., Jasinski, J. M., & Paty, C. (2025). Estimating soft X-ray emission from Uranus's magnetosheath. Journal of Geophysical Research: Space Physics, 130, e2025JA034171. https://doi.org/10.1029/2025JA034171
Omega Bands as a Source of Large dB/dt in the Dawn Sector
Omega Bands as a Source of Large dB/dt in the Dawn Sector
By Rosie Hodnett (University of Leicester)
Omega bands are a type of aurora which occur in the dawn sector and drift eastwards. They are often described as having a morphology similar to that of the Greek letter Ω. Omega bands have been shown to have the potential to cause geomagnetically induced currents, which are an important area of research as they are recognised as a hazard to our infrastructure, such as power grids.
In this study, we have examined an omega band event which occurred from 23 – 04 UT on 2012-11-13—14 using multiple instruments around Tromsø, Norway (69.6°N, 19.2°E). The first two panels (a-b) of the figure show EISCAT UHF/VHF electron density measurements, panel (c) shows a keogram of all-sky camera (ASC) data. It is clear that when the luminous aurora passes over head, enhancements in electron density are observed.
Panel (d) shows the magnetic field perturbations as measured by the IMAGE magnetometer and (e) shows dB/dt. For this event, we saw large perturbations in the Y component of the magnetic field, with a maximum peak of approx. 915 nT. The rapid motion of the omega bands leads to large dB/dt of above 10 nT/s.
Panel (f) shows AMPERE data, where the yellow dashed line is the location of EISCAT, where red is upward field aligned current (FAC) and blue is downward FAC. The auroral signatures and large dB/dt are evident when EISCAT is located between the boundary of region 1 and 2 current systems.
Panel (g) shows AL, where negative excursions due to the ground based magnetic perturbations of the omega bands are apparent. It is important that these rapid variations in AL are not misidentified as substorms, because as well as substorms, we have shown that omega band activity in the dawn sector causes drops in AL.
See publication for details:
Hodnett, R. M., Milan, S. E., Nozawa, S., Raita, T., Gjerloev, J. W., Vines, S. K., & Paxton, L. J. (2025). Omega bands as a source of large dB/dt in the dawn sector. Journal of Geophysical Research: Space Physics, 130, e2025JA034342. https://doi.org/10.1029/2025JA034342