Titans Haze: Uncertainties and Effects on Albedos

Titans Haze: Uncertainties and Effects on Albedos
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This research delves into Titan's haze, exploring its uncertainties and impact on derived surface albedos. The study sheds light on Titan's atmosphere, highlighting its composition, haze formation, and prebiotic potential. Through radiative transfer modeling and analysis of in-situ measurements, the findings reveal insights into the changing physical properties of Titan's haze and atmospheric circulation patterns. The study concludes with observations of increased particle size, challenging existing models and proposing selective circulation as a potential explanation.

  • Titan
  • Haze
  • Atmosphere
  • Albedos
  • Research

Uploaded on Feb 16, 2025 | 0 Views


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  1. Titans Haze Uncertainties and their Effects on Derived Surface Albedos Tymon Khamsi, Caitlin Griffith, Lyn Doose, Jake Turner, Paulo Penteado

  2. What/Where is Titan?

  3. Why Study Titans Atmosphere? Simpler model of earth Single circulation cell Methane cycle: analogous to Earth s water cycle Unexplained Methane Age of atmosphere unknown Without constant supply, liquid & atmospheric methane will break down within million years Formation vs. recent volcanism

  4. Titans Atmosphere 9.48% nitrogen 1.6% methane Methane photolysis forms hydrocarbon haze Responsible for orange appearance Possible prebiotic source Opaque to visible, near-IR wavelengths

  5. Approach Radiative Transfer spectra model (Griffith et al, 2011) Model parameters measured in situ by Huygens Probe (2005) Single Scattering Albedo Ratio of scattering to total extinction Optical Depth Low optical depth = high visibility (low chance of interaction) Haze Scaling Factor (hfac)

  6. Results Consistent with seasonal atmospheric circulation described in Rannou et. at. 2006

  7. Results/Analysis Possible explanation: haze physical properties are changing

  8. Results/Analysis Tried: increasing model s single scattering albedo parameter Question: what could cause more scattering and less extinction?

  9. Conclusions Increase in mean atmospheric particle size from 2005 2007 Current models do not account for this Possible explanation: selective circulation

  10. Acknowledgments Dr. Caitlin Griffith Paulo Penteado Robert Zellem Arizona Space Grant Consortium NASA The University of Arizona

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