Nature of the stratospheric haze on Uranus - Evidence for condensed hydrocarbons

Physics

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Atmospheric Models, Haze, Hydrocarbons, Stratosphere, Uranus Atmosphere, Aerosols, Atmospheric Chemistry, Particulates, Planetary Limb, Voyager 2 Spacecraft

Scientific paper

The characteristics and origin of lower-stratosphere haze on Uranus are investigated on the basis of high-phase-angle images obtained at 430-600 nm with the wide-angle and narrow-angle cameras of Voyager 2 during its encounter with Uranus in January 1986. The data-reduction and model-fitting procedures are explained in detail, and the results are presented in extensive tables and graphs. The data are found to be best matched by a haze consisting of particles of modal radius 130 + or - 20 nm and number density 2 + or - 1 per cu cm at the 44-mbar level; such aerosols could be formed by the stratospheric condensation of photochemically produced hydrocarbon gases (locally formed diacetylene and ethane, acetylene, and diacetylene formed at higher altitudes). A total aerosol production rate of (2-15) x 10 to the -17th g/sq cm sec is estimated.

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