Jupiter's shocking electrons may help explain how particles accelerate

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Electrons around Jupiter have been caught in the process of being accelerated, revealing a potentially unified explanation for particle acceleration, according to US scientists. They analysed data from NASA’s Juno spacecraft taken as it passed through a shockwave between Jupiter’s magnetosphere and the solar wind, known as Jupiter's bow shock. Shocks are disturbances that cause changes in pressure. In a region upstream of a collisionless shock - particle-based shocks which can cause cosmic rays to accelerate to near the speed of light - Juno recorded a foreshock, in which short-lived plasma structures accelerated particles. The team combined the Jupiter data with measurements from other planets, deriving a relationship between foreshock size and maximum particle energies. The authors say the size of foreshocks scales with the overall size of a shock system and sets a practical upper limit on the achievable particle energy. Future studies should test the universality of the proposed scaling, they conclude.

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From: Springer Nature

Observations of electron acceleration in Jupiter’s magnetic field

Electrons around Jupiter have been caught in the process of being accelerated, revealing a potentially unified mechanism for particle acceleration. The findings, published in Nature, may help constrain how energetic particles are produced throughout the Universe.

Shocks are disturbances created by a perturber/object/fluid moving through a fluid faster than the local speed of sound, causing an abrupt change in pressure at the boundary between the two. Typical examples are bow shocks where planetary atmospheres and solar winds meet, named after the analogous shocks produced on water by the bow of a ship. Most shocks in space plasma are collisionless, because particle densities are too low for direct collisions between particles to convert the shock's energy into heat. Instead, this is done by electromagnetic forces. Collisionless shocks are thought to be a site in which cosmic rays can accelerate to relativistic speeds (near the speed of light), a process known as relativistic electron acceleration. However, a lack of direct observational evidence has limited scientists’ understanding of how these structures work.

Savvas Raptis and colleagues analysed data from NASA’s Juno spacecraft taken as the probe traversed through a shockwave formed between Jupiter’s magnetosphere and the solar wind (Jupiter's bow shock). The instruments on Juno observed a foreshock, a region upstream of a collisionless shock spanning several of Jupiter's radii. Within this foreshock, transient plasma structures accelerated particles to relativistic speeds. The authors noticed that the size of such foreshocks scales with the overall size of a shock system and sets a practical upper limit on the achievable particle energy. By combining the Jupiter observations with existing measurements from other planets, the authors derive a relationship between foreshock transient size and maximum particle energies.

The study shows that planetary and heliophysics missions can provide crucial, observation-based constraints on particle acceleration theories. The authors note that extending the results to distant astrophysical shocks requires assumptions beyond direct measurement, and that further observations and modelling will be needed to test the universality of the proposed scaling.

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The acceleration process in an illustrative form
The acceleration process in an illustrative form

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Organisation/s: Johns Hopkins University, USA
Funder: S.R. acknowledges funding from the Johns Hopkins University Applied Physics Laboratory independent R&D fund. S.R. acknowledges E. Batziou, F. Driessen, A. Lalti and M. Lindberg for their discussions. S.R. also acknowledges the International Space Sciences Institute (ISSI) team 465: ‘Foreshocks Across the Heliosphere: System Specific or Universal Physical Processes?’, team 555: ‘Impact of Upstream Mesoscale Transients on the Near-Earth Environment’ and the NSF GEM Focus Group ‘Multiscale Dayside Transients and Their Effect on Earth’s Magnetosphere’. D.L.T. acknowledges support from the NSF and NASA research grants (NSF grant no. 2225463 and NASA grant no. 80NSSC24K0173). D.C. acknowledges support from NSF AST-2510951. J.R.S. acknowledges NFDAP grant no. 80NSSC23K0665. Finally, we acknowledge the entire Juno team and the instrument principal investigators for data access and support.
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