Investigating Boundary Layer Properties at Jupiter's Dawn Magnetopause

Abstract We survey crossings of Jupiter's dawn magnetopause during the Juno prime mission to identify and characterize Jupiter's magnetopause boundary layer. Using plasma and magnetic field observations from Jovian Auroral Distributions Experiment and Juno Magnetic Field investigation, we identify 53 boundary layer events from the 62 magnetopause crossings studied here. We find that the boundary layer generally exhibits mixed properties of magnetosheath and magnetosphere electron distributions, including lower characteristic electron energies and denser ion populations than in the magnetosphere, but higher characteristic electron energies and less dense ion populations than in the magnetosheath. Boundary layer proton speeds are on average slower than both the magnetosheath and magnetosphere. Other proton parameters in the boundary layer have intermediate values between the magnetosheath and magnetosphere. Through ion composition analysis in regions adjacent to the magnetopause, we find evidence of solar wind and magnetospheric plasma in the boundary layer that suggests plasma is transported across the magnetopause in both directions. This mass and energy transport may be the result of solar wind interactions such as magnetic reconnection and Kelvin‐Helmholtz instabilities. However, many boundary layer events do not exhibit local signatures of these solar wind interactions and plasma may be transported by a non‐local process or diffusively transported.

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Publication Details

Journal
Journal of Geophysical Research Space Physics
Published
2024-08-01
DOI
https://doi.org/10.1029/2024ja032926
Citations
1
Primary Topic
Astro and Planetary Science
Type
article
Field-Weighted Citation Impact
0.33

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article

Investigating Boundary Layer Properties at Jupiter's Dawn Magnetopause

F. Allegrini, F. Bagenal, Jake Montgomery, R. W. Ebert et al.
1 citations
Journal of Geophysical Research Space Physics
Astro and Planetary Science
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article

Investigating Boundary Layer Properties at Jupiter's Dawn Magnetopause

F. Allegrini, F. Bagenal, Jake Montgomery, R. W. Ebert, S. A. Fuselier, S. J. Bolton, J. R. Szalay, Robert J. Wilson
article en
1 citations

Abstract

Abstract We survey crossings of Jupiter's dawn magnetopause during the Juno prime mission to identify and characterize Jupiter's magnetopause boundary layer. Using plasma and magnetic field observations from Jovian Auroral Distributions Experiment and Juno Magnetic Field investigation, we identify 53 boundary layer events from the 62 magnetopause crossings studied here. We find that the boundary layer generally exhibits mixed properties of magnetosheath and magnetosphere electron distributions, including lower characteristic electron energies and denser ion populations than in the magnetosphere, but higher characteristic electron energies and less dense ion populations than in the magnetosheath. Boundary layer proton speeds are on average slower than both the magnetosheath and magnetosphere. Other proton parameters in the boundary layer have intermediate values between the magnetosheath and magnetosphere. Through ion composition analysis in regions adjacent to the magnetopause, we find evidence of solar wind and magnetospheric plasma in the boundary layer that suggests plasma is transported across the magnetopause in both directions. This mass and energy transport may be the result of solar wind interactions such as magnetic reconnection and Kelvin‐Helmholtz instabilities. However, many boundary layer events do not exhibit local signatures of these solar wind interactions and plasma may be transported by a non‐local process or diffusively transported.

Journal of Geophysical Research Space PhysicsVol. 129(8)
Southwest Research Institute (US), University of Colorado Boulder (US), Princeton University (US), Laboratory for Atmospheric and Space Physics (US), The University of Texas at San Antonio (US)
Aurora Foundation, Experiment
Affordable and clean energy
Openalex Percentile: Top 35%
Astro and Planetary Science
0.33
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