Auroral and Non‐Auroral H3+ Ion Winds at Uranus With Keck‐NIRSPEC and IRTF‐iSHELL

Emma Thomas*, Tom Stallard, Henrik Melin, M. Nahid Chowdhury, Luke Moore, James O'Donoghue, Rosie E. Johnson, Ruoyan Wang, Katie Knowles, Paola Tiranti, N. Dello Russo, Ronald J. Vervack, Hideyo Kawakita

*Corresponding author for this work

    Research output: Contribution to journalArticlepeer-review

    6 Downloads (Pure)

    Abstract

    To date, no investigation has documented ionospheric flows at Uranus. Previous investigations of Jupiter and Saturn have demonstrated that mapping ion winds can be used to understand ionospheric currents and how these connect to magnetosphere‐ionosphere coupling. We present a study of Uranus's near infrared emissions (NIR) using data from the Keck II Telescope's Near InfraRed SPECtrograph (NIRSPEC) and the InfraRed Telescope Facility's iSHELL spectrograph. H3+ emission lines were used to derive dawn‐to‐dusk intensity, ionospheric temperatures and ion densities to identify auroral emissions, with their Doppler shifts used to measure ion velocities. We confirm the presence of the southern NIR aurora in 2016, driven by elevated H3+ column densities up to 6.0 × 1016 m−2. While no auroral emissions were detected in 2014, we find a 14%–20% super rotation across the planet's disk in 2014 and a 7%–18% super rotation in 2016.
    Original languageEnglish
    Article numbere2024GL112001
    Number of pages9
    JournalGeophysical Research Letters
    Volume52
    Issue number7
    Early online date1 Apr 2025
    DOIs
    Publication statusPublished - 16 Apr 2025

    Keywords

    • H3+
    • Uranus
    • ground‐based astronomy
    • ice giant ionosphere
    • infrared aurorae
    • infrared spectrscopy
    • H
    • ground-based astronomy

    Cite this