4.5 Article

Modeling the Jovian magnetic field and its secular variation using all available magnetic field observations

期刊

JOURNAL OF GEOPHYSICAL RESEARCH-PLANETS
卷 121, 期 3, 页码 309-337

出版社

AMER GEOPHYSICAL UNION
DOI: 10.1002/2015JE004951

关键词

Jupiter; magnetic field; secular variation

资金

  1. Leverhulme Trust [F/00 025/AI]
  2. NERC [bgs05003] Funding Source: UKRI
  3. Natural Environment Research Council [bgs05003] Funding Source: researchfish

向作者/读者索取更多资源

We present new models of Jupiter's internal magnetic field and secular variation from all available direct measurements from three decades of spacecraft observation. A regularized minimum norm approach allows the creation of smooth, numerically stable models displaying a high degree of structure. External field from the magnetodisk is modeled iteratively for each orbit. Jupiter's inner magnetosphere is highly stable with time, with no evidence for variation with solar activity. We compare two spherical harmonic models, one assuming a field constant in time and a second allowing for linear time variation. Including secular variation improves data fit with fewer additional parameters than increasing field complexity. Our favored solution indicates a approximate to 0.012%yr(-1) increase in Jupiter's dipole magnetic moment from 1973 to 2003; this value is roughly one quarter of that for Earth. Inaccuracies in determination of the planetary reference frame cannot explain all the observed secular variation. Should more structure be allowed in the solutions, we find the northern hemispherical configuration resembles recent models based on satellite auroral footprint locations, and there is also evidence of a possible patch of reversed polar flux seen at the expected depth of the dynamo region, resembling that found at Earth and with implications for the Jovian interior. Finally, using our preferred model, we infer flow dynamics at the top of Jupiter's dynamo source. Though highly speculative, the results produce several gyres with some symmetry about the equator, similar to those seen at Earth's core-mantle boundary, suggesting motion on cylinders aligned with the rotation axis.

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