Observationally measuring the location of the H 2 O snowline is crucial for understanding the planetesimal and planet formation processes, and the origin of water on Earth. In disks around Herbig Ae stars (T * ∼10,000K, M * 2.5M ), the position of the H 2 O snowline is further from the central star compared with that around cooler, and less massive T Tauri stars. Thus, the H 2 O emission line fluxes from the region within the H 2 O snowline are expected to be stronger. In this paper, we calculate the chemical composition of a Herbig Ae disk using chemical kinetics. Next, we calculate the H 2 O emission line profiles, and investigate the properties of candidate water lines across a wide range of wavelengths (from mid-infrared to sub-millimeter) that can locate the position of the H 2 O snowline. Those line identified have small Einstein A coefficients (∼ 10 −6 − 10 −3 s −1 ) and relatively high upper state energies (∼ 1000K). The total fluxes tend to increase with decreasing wavelengths. We investigate the possibility of future observations (e.g., ALMA, SPICA/SMI-HRS) to locate the position of the H 2 O snowline. Since the fluxes of those identified lines from Herbig Ae disks are stronger than those from T Tauri disks, the possibility of a successful detection is expected to increase for a Herbig Ae disk.