P074-06
Measuring the Stratospheric Temperature of Uranus Using Archival Stellar Occultations
Abstract:
Aims: When the atmosphere of Uranus was last sampled, significant disagreements in temperatures were found between different methods of detection—as much as hundreds of Kelvin. We endeavor to use updated occultation analysis techniques (inversion) [5, 6] on archival data to help resolve the stratospheric temperature uncertainty. By producing higher resolution profiles, we can search for wave action, a potential source of heating that could help move toward resolving the energy crisis [7].
Methods: Starting with a boundary condition and assumptions of atmospheric properties, the inversion procedure performs an Abel transform point-by-point down each occultation light curve. Each point samples a different radius of intervening atmosphere and returns temperature, pressure and neutral density, with errors. We use as many archival datasets as possible to strengthen findings and search for wave activity following [8].
Results: We present high-resolution atmospheric profiles, compare to original analyses as well as other archival remote-sensing results and re-state the stratospheric temperature discrepancy. We outline the stellar occultation observations that should occur in the coming years in advance of potential mission planning for a planetary encounter with the Ice Giants.
[1] Li, C. et al. 2018
[2] Marley & McKay 1999
[3] Pearl et al. 1990
[4] West et al. 1987
[5] Elliot & Young 1992
[6] Elliot, Person, & Qu 2003
[7] Mueller-Wodarg 2008
[8] Saunders, Person, & Withers, in review