EPSC Abstracts
Vol. 18, EPSC-DPS2025-1239, 2025, updated on 09 Jul 2025
https://doi.org/10.5194/epsc-dps2025-1239
EPSC-DPS Joint Meeting 2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Determination of Jupiter’s Primordial Radius, Accretion Rate, and Magnetic Field
Konstantin Batygin1 and Fred Adams2
Konstantin Batygin and Fred Adams
  • 1Caltech, Geological & Planetary Sciences, Pasadena, United States of America (k.batygin@gmail.com)
  • 2Physics Department, University of Michigan, Ann Arbor, USA

Jupiter's formation significantly influenced the structure and evolution of our solar system, yet crucial details about its earliest physical state remain uncertain due to the complexity of planet-formation models. Here we will discuss Jupiter's primordial physical state by leveraging the dynamical history of Jupiter’s innermost satellites and the planet’s angular momentum budget. In particular, our analysis indicates that at the time the solar nebula dispersed, Jupiter was 2 to 2.5 times its current size. Furthermore, during this epoch, Jupiter had a magnetic field of at least ~200G, and it was accreting gas through a circumplanetary disk at a rate of about one to two Jupiter masses per million years. These findings support core-accretion models of giant planet formation and offer a critical snapshot of Jupiter's properties at a pivotal stage of the solar system's evolution, providing new insights into the conditions that shaped the largest planet of the sun's planetary album.

How to cite: Batygin, K. and Adams, F.: Determination of Jupiter’s Primordial Radius, Accretion Rate, and Magnetic Field, EPSC-DPS Joint Meeting 2025, Helsinki, Finland, 7–12 Sep 2025, EPSC-DPS2025-1239, https://doi.org/10.5194/epsc-dps2025-1239, 2025.