EPSC Abstracts
Vol. 18, EPSC-DPS2025-1363, 2025, updated on 14 Jul 2025
https://doi.org/10.5194/epsc-dps2025-1363
EPSC-DPS Joint Meeting 2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Pluto’s Atmosphere in Decline
Amanda Sickafoose1, Michael Person2, Carlos Zulaaga2, Stephen Levine3, Timothy Brothers2, Bastian Knieling4, Tim Lister5, David Osip6, Patricio Rojo7, Karsten Schindler4, Joseph Brimacombe8, Tim Carruthers8, Abigail Colclasure2, Petro Janse van Rensburg9,10, Anja Genade9,10, and Stephen Potter9,11
Amanda Sickafoose et al.
  • 1Planetary Science Institute, Tucson, AZ, U.S.A. (asickafoose@psi.edu)
  • 2Massachusetts Institute of Technology, Cambridge, MA, U.S.A. (mjperson@mit.edu; czuluaga@mit.edu; bro@mit.edu)
  • 3Lowell Observatory, Flagstaff, AZ, U.S.A. (sel@lowell.edu)
  • 4Institute of Space Systems, Universität Stuttgart, Stuttgart, Germany (bknieling@dsi.uni-stuttgart.de; schindler@dsi.uni-stuttgart.de)
  • 5Las Cumbres Observatory, Goleta, CA, U.S.A. (tlister@lco.global)
  • 6Carnegie Observatories, Pasadena, CA, U.S.A. (dosip@carnegiescience.edu)
  • 7Departmento de Astronomia, Universidad de Chile, Santiago, Chile (pato@das.uchile.cl)
  • 8Savannah Skies Observatory, Chillagoe, Australia (jbrimaco@bigpond.net.au; tim@astrophoto.com.au)
  • 9South African Astronomical Observatory, Observatory, South Africa (petro@saao.ac.za; genadeanja@gmail.com; sbp@saao.ac.za)
  • 10Department of Astronomy, University of Cape Town, Rondebosch, South Africa
  • 11Department of Physics, University of Johannesburg, Johannesburg, South Africa

Pluto is the only minor planet (excluding satellites) that is known to host a thin, global atmosphere. The atmosphere has microbar-level surface pressure, is composed primarily of nitrogen, and contains a layered haze made of organic materials (e.g. Gladstone et al., 2016, Science, 351, id. aad8866). Notably, Pluto’s atmosphere is intricately linked to its surface ices through vapor-pressure equilibrium (e.g. Elliot et al., 1989, Icarus, 77, 148). Because of the strong tie between the atmosphere and ices, the surface pressure is highly dependent on ice temperature, which is a function of orbital and seasonal timescales. On Pluto, with an eccentric orbit (e = 0.25) and high obliquity (~123 deg.), these changes are pronounced and the atmospheric properties can vary significantly on timescales of only a few decades. Thermophysical, volatile-transport models have been developed to study Pluto’s atmospheric evolution; predictions range from atmospheric contraction or collapse over the coming decades to an atmosphere that remains throughout Pluto’s entire revolution around the Sun (e.g. Young, 2013, ApJ Lett., 766, L22; Hansen et al. 2015, Icarus, 246, 183; Bertrand et al. 2018, Icarus, 309, 277; Johnson et al. 2021, Icarus, 356, id.114070).

Stellar occultation data are the most direct way to measure Pluto’s atmosphere from the Earth. Results from previous occultations reported that Pluto’s atmospheric pressure monotonically increased since its definitive discovery in 1988 through 2016 (Meza et al. 2019, A&A, 625, id.A136) and then that the atmosphere had possibly begun freezing out in 2018-2019 (Arimatsu et al. 2020, A&A 638, L5; Young et al. 2021, AAS DPS Meeting #53, id.307.06). Observations of an occultation in 2020 did not show a pressure drop and were interpreted to be either a continued pressure increase (Poro et al. 2021, A&A, 652, L7) or a plateau phase (Sicardy et al. 2021, ApJ Lett, 923, L31). Here, we report results from ten successfully-observed stellar occultations by Pluto between 2017 August and 2023 July that have not yet been published. The stellar magnitudes ranged from G=12.91 to 18.4 with geocentric relative velocities between 1.7 and 24.5 km/s.  Four of these events had successful chords from multiple sites, while six events were from single sites. We carried out atmospheric fits assuming clear, isothermal atmospheres as well as atmospheres with a haze layer. Our results indicate that Pluto’s atmospheric pressure has begun decreasing in recent years.

This work is supported by NASA grant 80NSSC21K043.

How to cite: Sickafoose, A., Person, M., Zulaaga, C., Levine, S., Brothers, T., Knieling, B., Lister, T., Osip, D., Rojo, P., Schindler, K., Brimacombe, J., Carruthers, T., Colclasure, A., Janse van Rensburg, P., Genade, A., and Potter, S.: Pluto’s Atmosphere in Decline, EPSC-DPS Joint Meeting 2025, Helsinki, Finland, 7–12 Sep 2025, EPSC-DPS2025-1363, https://doi.org/10.5194/epsc-dps2025-1363, 2025.