4.5 Article

Auroral evidence of radial transport at Jupiter during January 2014

Journal

JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS
Volume 121, Issue 10, Pages 9972-9984

Publisher

AMER GEOPHYSICAL UNION
DOI: 10.1002/2016JA023007

Keywords

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Funding

  1. STFC [ST/I004084/1, ST/N000722/1]
  2. RAS fellowship
  3. National Science Foundation [1524651]
  4. PRODEX program
  5. STFC Ernest Rutherford Fellowship
  6. Science and Technology Facilities Council [1481302, ST/I004084/1] Funding Source: researchfish
  7. STFC [ST/I004084/1] Funding Source: UKRI
  8. Grants-in-Aid for Scientific Research [26287118] Funding Source: KAKEN
  9. Div Atmospheric & Geospace Sciences
  10. Directorate For Geosciences [1524651] Funding Source: National Science Foundation

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We present Jovian auroral observations from the 2014 January Hubble Space Telescope (HST) campaign and investigate the auroral signatures of radial transport in the magnetosphere alongside contemporaneous radio and Hisaki EUV data. HST FUV auroral observations on day 11 show, for the first time, a significantly superrotating polar spot poleward of the main emission on the dawnside. The spot transitions from the polar to main emission region in the presence of a locally broad, bright dawnside main emission feature and two large equatorward emission features. Such a configuration of the main emission region is also unreported to date. We interpret the signatures as part of a sequence of inward radial transport processes. Hot plasma inflows from tail reconnection are thought to flow planetward and could generate the superrotating spot. The main emission feature could be the result of flow shears from prior hot inflows. Equatorward emissions are observed. These are evidence of hot plasma injections in the inner magnetosphere. The images are thought to be part of a prolonged period of reconnection. Radio emissions measured by Wind suggest that hectometric (HOM) and non-Io decametric (DAM) signatures are associated with the sequence of auroral signatures, which implies a global magnetospheric disturbance. The reconnection and injection interval can continue for several hours.

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