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Modeling Titan’s Planetary Boundary Layer at the Huygens Landing Site: Evidence for the Role of Subsurface Methane Evaporation in Limiting Convective Growth

  • Authors: Victoria L. Hartwick, Scot C. R. Rafkin, Alejandro Soto

Victoria L. Hartwick et al 2026 The Planetary Science Journal 7 .

  • Provider: AAS Journals

Caption: Figure 16.

Diurnal integrated (a) sensible heat flux [MJ m−2], (b) latent heat flux [MJ m−2], and (c) methane evaporation [kg m−2] for all moist regolith simulations. The gray band shows the approximate target diurnal maximum PBL depth (600–1200 m). Icons distinguish between different methane evaporation schemes (triangle: MRPS; square: NSMT; circle: SPS). Colors indicate different Tsol.

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