Titan

THUNDER: A Titan Orbiter Mission Concept for the New Frontiers Program Designed at the JPL Planetary Science Summer School

By Keith Cowing
Status Report
The Planetary Science Journal
March 4, 2025
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THUNDER: A Titan Orbiter Mission Concept for the New Frontiers Program Designed at the JPL Planetary Science Summer School
THUNDER

Saturn’s moon Titan is an enigmatic icy world whose surface is constantly modified by its active, Earthlike precipitation system. Here, we propose the Titan’s Hydrocarbons: Uncovering New Dimensions of Evolutionary pRocesses (THUNDER) mission concept to investigate how Titan’s surface reflects the nature of its interior and its active hydrocarbon cycle.

This mission will change our understanding of Titan’s surface through three science objectives: characterizing the heat and material transport properties of Titan’s icy outer layer, tracing surface liquid storage through and across the crust, and assessing the total hydrocarbon budget through time.

This New Frontiers-class mission, designed as part of the Jet Propulsion Laboratory Planetary Science Summer School, responds directly to the call for a Titan orbiter in the NASA Planetary Science and Astrobiology Decadal Survey 2023–2032. THUNDER’s focused geology and geophysics mission could achieve full surface mapping to complement both the Cassini–Huygens and Dragonfly missions using gravity science, radar with three operational modes, and a visible-to-infrared spectrometer.

These instruments together could give us the first look at Titan as a fully connected and geologically active world, revolutionizing our understanding of icy bodies, fluvial and atmospheric processes, and habitability across geologic time.

Here, we summarize the goals of the science mission and engineering approaches, as well as challenges and future directions to study before THUNDER can become a viable mission concept.

Schematic showing the two end members for the state of Titan’s ice shell. (a) Convecting ice shell, with a thick convective layer underlying a thin conducting layer. (b) Purely conductive ice shell, made up of only a thin conductive layer. Note that only the features we aim to test here are present in the graphic; the existence of clathrate layers, finer-scale interior shell structures, and any further solid layers may certainly be present within Titan, but are not depicted.– The Planetary Science Journal

Cassandra Seltzer, Rudi Lien, Brandon T. Radzom, Ella Mullikin, Kimberly Bott, Gwendolyn Brouwer, David G. Burtt, Chloe Gentgen, Jewel Abbate, Victor Gandarillas, Austin P. Green, Tristen Head, Jonathon R. Hill, Jennifer N. Larson, Nicholas J. Montiel, M. Regina A. Moreno, Nicholas L. Wagner, Piyumi Wijesekara, James Tuttle Keane, Alfred E. Nash and Jennifer Scully

THUNDER: A Titan Orbiter Mission Concept for the New Frontiers Program Designed at the JPL Planetary Science Summer School, The Planetary Science Journal, (Open Access)

Astrobiology

Explorers Club Fellow, ex-NASA Space Station Payload manager/space biologist, Away Teams, Journalist, Lapsed climber, Synaesthete, Na’Vi-Jedi-Freman-Buddhist-mix, ASL, Devon Island and Everest Base Camp veteran, (he/him) 🖖🏻