Forward Modeling of 3‐D Ion Properties in Jupiter’s Magnetosphere Using Juno/JADE‐I Data

Author:

Wang Jian‐zhao12ORCID,Bagenal Fran1ORCID,Wilson Robert J.1ORCID,Nerney Edward1,Crary Frank1ORCID,Dols Vincent1ORCID,Ebert Rob W.34ORCID,Valek Phil W.3ORCID,Allegrini Frederic3ORCID,Kim Thomas K.5ORCID,Szalay Jamey R.6ORCID

Affiliation:

1. Laboratory for Atmospheric and Space Physics University of Colorado Boulder Boulder CO USA

2. Department of Astrophysical and Planetary Sciences University of Colorado Boulder Boulder CO USA

3. Southwest Research Institute San Antonio TX USA

4. University of Texas at San Antonio San Antonio TX USA

5. Space Science and Applications Los Alamos National Laboratory Los Alamos NM USA

6. Department of Astrophysical Sciences Princeton University Princeton NJ USA

Abstract

AbstractThe Jovian Auroral Distributions Experiment Ion sensor (JADE‐I) on NASA’s Juno mission provides in‐situ measurements of ions from 0.1 to 46.2 keV/q inside Jupiter’s magnetosphere. JADE‐I is used to study the plasma with two types of datasets from the same measurement: Time‐of‐flight (TOF) and SPECIES. The TOF dataset provides mass‐per‐charge measurements with a range of 1–64 amu/q but oversamples particles over 6π steradian viewing per spacecraft spin and has little directional information. On the other hand, the SPECIES dataset can provide a good measurement of the flow direction but does not provide mass‐per‐charge information due to the telemetry limit. In this study, we developed a 2‐step forward modeling method that combines the advantages and avoids the disadvantages of TOF and SPECIES data to derive the 3‐D properties of heavy ions. Assuming that the ion velocity distribution can be described with the kappa distribution, we first perform the forward model fit of the TOF data to calculate the relative abundance of heavy ion species. Then we fix the relative abundance and perform the second forward model fit on the SPECIES data. Using this method, we obtain the densities of different heavy ions, the shared temperature and kappa value, and the 3‐D flow velocity vector. Some data examples of the equatorial plasma disk before Perijove 24 are included to demonstrate the method. Plasma properties can then be mapped to explore spatial and temporal variabilities in Jupiter’s magnetosphere.

Publisher

American Geophysical Union (AGU)

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