A physical model of Titan's aerosols

Physics

Scientific paper

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Aerosols, Atmospheric Models, Atmospheric Physics, Satellite Atmospheres, Titan, Albedo, Atmospheric Composition, Haze, Optical Thickness, Particle Size Distribution, Size Determination, Vertical Distribution

Scientific paper

A modeling effort is presented for the nature of the stratospheric haze on Titan, under several simplifying assumptions; chief among these is that the aerosols in question are of a single composition, and involatile. It is further assumed that a one-dimensional model is capable of simulating the general characteristics of the aerosol. It is suggested in this light that the detached haze on Titan may be a manifestation of organized, Hadley-type motions above 300 km altitude, with vertical velocities of 1 cm/sec. The hemispherical asymmetry of the visible albedo may be due to organized vertical motions within the upper 150-200 km of the haze.

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