Characterising injection signatures in Jupiter's ultraviolet aurora using Juno observations
Linus Head, Denis Grodent, Bertrand Bonfond, Alessandro Moirano, Guillaume Sicorello, Julie Vinesse, Alyssa Mouton, Maïté Dumont, Thomas Greathouse, Vincent Hue, Ali Sulaiman, Barry Mauk, Zhonghua Yao, Ruilong Guo, Jinyan Zhao
TL;DR
The study addresses whether Jupiter's ultraviolet injection signatures originate from magnetodisc scattering or high-latitude Alfvénic acceleration and whether outer arcs are related to injections. It combines automatic detection of discrete UV features from Juno-UVS with in-situ measurements (JEDI, MAG-FGM) to test mechanisms and to classify injections into dawn-storm and non-dawn-storm types, uncovering strong evidence for magnetodisc-pitch-angle scattering as the dominant driver and arsenals of energy-dependent drift shaping feature morphology. A key finding is that the hemispheric power ratio follows the isotropic-scattering relation $\log_{2}\left(\frac{P_{N}}{P_{S}}\right) = -\log_{2}\left(\frac{B_{N}}{B_{S}}\right)$ with substantial scatter partly explained by slight sub-corotation of injections (≈85%), and that arc-like outer features can be sequences of dawn-storm injections broadened by drift. Arc-like features and blob-like injections share similar particle/wave properties, suggesting a common origin, with arc formation arising from energy-dependent drift rather than a distinct acceleration mechanism, and non-dawn-storm injections contributing to a broad, often-dusk-dominated distribution of injections.
Abstract
Discrete features in Jupiter's ultraviolet aurora have been interpreted as signatures of plasma injections in the middle magnetosphere. There exists some ambiguity whether magnetodisc scattering or high-latitude Alfvenic acceleration best describes the observed properties of these injection signatures, and also to what extent arcs in the outer emission are related to injections. Many injection signatures are the result of the evolution of dawn storms; there is, however, limited evidence that non-dawn-storm injection signatures are sometimes present in the aurora. We use automatic detection of these discrete features, alongside data from Juno-UVS and in-situ measurements by other Juno instruments, to show that scattering likely accounts for most of the electron precipitation associated with injection signatures. Additionally, there is evidence that injection signatures can be classified into two types: dawn-storm and non-dawn-storm. Arc-like features in the outer emission show very similar properties to traditional blob-like injection signatures and may consist of sequences of injection signatures that have broadened into an arc via energy-dependent electron drift.
