4.5 Article

Saturn's Nightside Ring Current During Cassini's Grand Finale

Journal

Publisher

AMER GEOPHYSICAL UNION
DOI: 10.1029/2020JA028605

Keywords

Cassini; ring current; Saturn

Funding

  1. STFC Consolidated Grant [ST/N000749/1, ST/N000692/1]
  2. Royal Society Research Professorship
  3. STFC Quota Studentship [ST/N504117/1]
  4. Royal Society Wolfson Research Merit Award
  5. STFC [ST/N000692/1, ST/S000429/1] Funding Source: UKRI

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The study shows that the response of the ring current to solar wind conditions is influenced by the relative phasing of the two planetary period oscillations. A thick partial ring current is formed on the nightside during solar wind compressions when the PPOs are in antiphase, while it is not detected during compressions when the PPOs are in phase.
During Cassini's Grand Finale proximal orbits, the spacecraft traversed the nightside magnetotail to similar to 21 Saturn radii. Clear signatures of Saturn's equatorial current sheet are observed in the magnetic field data. An axisymmetric model of the ring current is fitted to these data, amended to take into account the tilt of the current layer by solar wind forcing, its teardrop-shaped nature and the magnetotail and magnetopause fringing fields. Variations in ring current parameters are examined in relation to external driving of the magnetosphere by the solar wind and internal driving by the two planetary period oscillations (PPOs), and compared with previous dawn and dayside observations. We find that the relative phasing of the PPOs determines the ring current's response to solar wind conditions. During solar wind compressions when the PPOs are in antiphase, a thick partial ring current is formed on the nightside, dominated by hot plasma injected by tail reconnection. This partial ring current should close partly via magnetopause currents and possibly via field-aligned currents into the ionosphere. However, during solar wind compressions when the PPOs are in phase, this partial ring current is not detected. During solar wind rarefactions an equatorial magnetodisc configuration is observed in the dayside/dawn/nightside regions, with similar total currents flowing at these local times. During very quiet intervals of prolonged solar wind rarefaction, a thin current sheet with an enhanced current density is formed, indicative of a ring current dominated by cool, dense, Enceladus water group ions.

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