The Astrophysical Journal · 1979 · 24 citations · 0 references
Natural SciencesAstronomyEarth SciencesPlanetary AstronomyPlanetary ScienceRemote SensingAtmospheric OpticsInterferometryPlanetary AlbedoPlanetary Remote SensingPlanetary SurfacesPlanetary TopographyAlbedoAlbedo MappingGeometric AlbedoPlanetary Mass DeterminationPlanetary Mass DistributionSpeckle InterferenceSpeckle InterferometrySurface Albedo Estimation
For the diameter of Pluto the values of 3000 + or - 400 km, assuming no limb darkening, and 3600 + or - 400 km, assuming limb darkening following a cosine law are obtained. The presence of a degree of limb darkening is possibly indicated by earlier work. The data also show evidence of surface structure, and possibly a strong surface mottling, strong central enhancement in brightness (as would be produced by a semispecular surface), or a combination of both. Values for the average geometric albedo are 0.36 + or - 0.14 (no limb darkening) and 0.25 + or - 0.08 (limb darkening included), consistent with a surface having a large covering of methane frost. From a determination of Pluto's mass using recent data, mean densities of 0.8 (+0.6, -0.3) g/cu cm (no limb darkening) and 0.5 (+0.3, -0.2) g/cu cm (limb darkening included) are obtained. Such low densities suggest that Pluto consists mainly of frozen volatiles.