A number of experimental and theoretical studies have suggested that the surface of water-ice is liquidlike. Ions in a liquidlike layer should be hydrated, whereas they are included in a salt crystal if the surface of ice is solidlike. Thus, the local structure of an ion can be a useful probe for the state of the ice surface. X-ray absorption fine structure has allowed us to determine the local structures of Brin the bulk and on the surface of water-ice simply by adjusting the incident angle of X-ray. In the bulk of ice doped with RbBr of g3 mM, Bris present in the crystal lattice of RbBr below the eutectic point (t eu ), but is completely hydrated above t eu . However, a higher transition temperature has been found for 1 mM RbBr, and, in addition, the hydration structure of Bris kept even at the temperatures lower than t eu . In contrast, the spectra for Brobtained from the surface of doped-ice involve strong contributions from the RbBr crystal even above t eu . Thus, against the expectation from the surface liquid layer on pure ice, the surface of RbBr-doped ice is waterless compared to its bulk as far as ion hydration is concerned. The spectra on the surface suggest some specific structures at higher temperatures, where the contribution from the crystal should become marginal because of the complete dissolution of RbBr in a solution phase. These specific spectral features can be successfully explained assuming the formation of a 1D RbBr crystal with hydrated Rb + .