Study of the vertical structure of Saturn's atmosphere using HST/WFPC2 images

Details Study of the vertical structure of Saturn's atmosphere using HST/WFPC2 images Study of the vertical structure of Saturn's atmosphere using HST/WFPC2 images

Jun 2004

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2004icar..169..413m&link_type=abstract

Icarus, Volume 169, Issue 2, p. 413-428.

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11

Saturn Atmosphere, Atmospheres Structure, Radiative Transfer

Scientific paper

We have studied the vertical structure of hazes at six different latitudes (-60°, -50°, -30°, -10°, +30°, and +50°) on Saturn's atmosphere. For that purpose we have compared the results of our forward radiative transfer model to limb-to-limb reflectivity scans at four different wavelengths (230, 275, 673.2, and 893 nm). The images were obtained with the Hubble Space Telescope Wide Field Planetary Camera 2 in September 1997, during fall on Saturn's northern hemisphere. The spatial distribution of particles appears to be very variable with latitude both in the stratosphere and troposphere. For the latitude range +50° to -50°, an atmospheric structure consisting of a stratospheric haze and a tropospheric haze interspersed by clear gas regions has been found adequate to explain the center to limb reflectivities at the different wavelengths. This atmospheric structure has been previously used by Ortiz et al. (1996, Icarus 119, 53-66) and Stam et al. (2001, Icarus 152, 407-422). In this work the top of the tropospheric haze is found to be higher at the southern latitudes than at northern latitudes. This hemispherical asymmetry seems to be related to seasonal effects. Different latitudes experience different amount of solar insolation that can affect the atmospheric structure as the season varies with time. The haze optical thickness is largest (about 30 at 673.2 nm) at latitudes +/-50 and -10 degrees, and smallest (about 18) at +/-30 degrees. The stratospheric haze is found to be optically thin at all studied latitudes from -50 to +50 degrees being maximum at -10° (τ=0.033). At -60° latitude, where the UV images show a strong darkening compared to other regions on the planet, the cloud structure is remarkably different when compared to the other latitudes. Here, aerosol and gas are found to be uniformly mixed down to the 400 mbar level.

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