We study the spectrophotometric properties of dwarf planet Ceres in the VIS-IR spectral range by means of hyper-spectral images acquired by the VIR imaging spectrometer on board the NASA Dawn mission. Disk-resolved observations with a phase angle within the interval were used to characterize Ceres’ phase curve in the 0.465-4.05 m spectral range. Hapke’s model was applied to perform the photometric correction of the dataset, allowing us to produce albedo and color maps of the surface. The -band magnitude phase function of Ceres was fitted with both the classical linear model and H-G formalism. The single-scattering albedo and the asymmetry parameter at 0.55m are and , respectively (two-lobe Henyey-Greenstein phase function); the modeled geometric albedo is ; the roughness parameter is . Albedo maps indicate small variability on a global scale with an average reflectance of . Isolated areas such as the Occator bright spots, Haulani, and Oxo show an albedo much higher than average. We measure a significant spectral phase reddening, and the average spectral slope of Ceres’ surface after photometric correction is and at VIS and IR wavelengths, respectively. Broadband color indices are and . H-G modeling of the -band magnitude phase curve for gives and , while the classical linear model provides and . The comparison with spectrophotometric properties of other minor bodies indicates that Ceres has a less back-scattering phase function and a slightly higher albedo than comets and C-type objects. However, the latter represents the closest match in the usual asteroid taxonomy.

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