Revealing the Local Time Structure of the Alfvén Radius and Travel Times in Jupiter's Magnetosphere

Jenkins, A. and Ray, L. C. and Fell, T. and Badman, S. V. and Lorch, C. T. S. (2024) Revealing the Local Time Structure of the Alfvén Radius and Travel Times in Jupiter's Magnetosphere. Journal of Geophysical Research: Planets, 129 (10): e2024JE008. ISSN 2169-9100

Abstract

Jovian magnetospheric plasma is coupled to the ionosphere through Alfvén waves. Alfvén waves enable the transport of angular momentum and energy between the planet and magnetospheric plasma, a process that ultimately generates Jupiter's bright auroral emissions. However, past the Alfvén radius, the location where the radial velocity is greater than the Alfvén velocity, magnetospheric plasma is decoupled from the planet. Alfvén waves launched by magnetospheric plasma do not reach the ionosphere, angular momentum cannot be transported from the planet, and auroral emissions should diminish. Knowledge of Jupiter's Alfvén radius location is critical for interpreting drivers of auroral emissions, in situ data, and applications of numerical models. Previous studies that determined the location of the Alfvén radius assumed an azimuthally symmetric magnetosphere and local‐time independent magnetic field. Here, we employ a statistical description of the magnetic field that includes local time effects. We find a minimum Alfvén radius of 30 R J ${\mathrm{R}}_{J}$ (Jupiter radii) at 6 LT, with plasma decoupled from the planet in the post‐dusk through dawn sector. Furthermore, no Alfvén radius exists within 60 R J ${\mathrm{R}}_{J}$ between 8 and 20 LT. At distances greater than 50 R J ${\mathrm{R}}_{J}$ , the Alfvén travel time is such that magnetospheric plasma moves substantially in the magnetosphere before angular momentum can be efficiently transferred from the atmosphere. Therefore, the angular momentum supplied may no longer be sufficient for the local conditions. Our results highlight the importance of local time considerations and offer new interpretations for local time dependent auroral features, such as the polar collar.