Hourly Periodic Variations of Ultralow‐Frequency (ULF) Waves in Jupiter's Magnetosheath

Author:

Gu W. D.12,Yao Z. H.123ORCID,Pan D. X.4ORCID,Xu Y.12ORCID,Zhang B.5ORCID,Delamere P. A.6ORCID,Fu S. Y.7ORCID,Xie L.7ORCID,Ye S. Y.8,Chen Y. N.8ORCID,Dunn W. R.3ORCID,Wei Y.12ORCID

Affiliation:

1. Key Laboratory of Earth and Planetary Physics Institute of Geology and Geophysics Chinese Academy of Sciences Beijing China

2. College of Earth and Planetary Sciences University of Chinese Academy of Sciences Beijing China

3. Mullard Space Science Laboratory University College London Dorking UK

4. School of Geophysics and Information Technology China University of Geosciences (Beijing) Beijing China

5. Department of Earth Sciences the University of Hong Kong Hong Kong China

6. Geophysical Institute University of Alaska Fairbanks AK Fairbanks USA

7. School of Earth and Space Sciences Peking University Beijing China

8. Department of Earth and Space Sciences Southern University of Science and Technology Shenzhen China

Abstract

AbstractPeriodic variations are widely identified in the Jovian system, varying from 10 s of seconds to several days or even longer. These processes are strongly influenced by solar wind conditions, planetary rotation and Io's volcanic activity. Ultralow‐frequency (ULF) waves at 10 s of minutes, which are the typical time scale of field‐line resonance, are considered as a crucial process in driving the Jovian energy circulation. The longer time‐scale periodicities are likely associated with global mass circulation. In this study, we focus on multihour variations of the ULF wave energy, which are difficult to identify within the magnetosphere due to the rapid planetary rotation modulation. Using the magnetic field observations from Juno and Galileo in Jupiter's magnetosheath, we found multiple significant multihour periodicities, widely distributed from 2 to 10 hr, peaked at different values from case to case. The most common periodicities were between 3 and 5 hr, existing in both the dawn and dusk sides. These common periodicities are likely associated with the energy transport from the inside to the magnetosheath.

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

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