Investigating Pluto's lower atmosphere from a central-flash stellar occultation

Physics

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Scientific paper

A central-flash occultation is visible when the observer is located near the center of the shadow path. In 2007, we observed a stellar occultation from four sites from New Zealand and Australia. One of our sites, Mt. John Observatory, was 70 km from the shadow center and observed a central flash. Due to the large aperture and predicted near central location for this site, we chose to carry out a dual-wavelength observation from Mt. John Observatory. The centralflash observations for both the blue and red channels were very similar in structure and amplitude. We have modeled the central flash assuming either a haze layer or a thermal gradient. For the haze-only model, the rays contributing to the central flash come from an altitude of 1130 km. This altitude is much less than the current best estimate for Pluto's radius. For this reason, the purely refractive solution (thermal gradient) is preferred to the extinction only solution (haze layer). A thermal gradient of 5 K/km fits the flux level and an ellipticity of 0.085 and a nearly prolate orientation match the separation and relative strength of the two peaks. Intermediate solutions with some haze and some thermal gradient are possible.

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