Candidate Water Vapor Lines to Locate the H$_{2}$O Snowline through High-Dispersion Spectroscopic Observations II. The Case of a Herbig Ae Star
Abstract: 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 ($T{\mathrm{}}\sim$ 10,000K, $M_{\mathrm{}}\gtrsim$ 2.5$M_{\bigodot}$), 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 ($\sim 10{-6} -10{-3}$ s${-1}$) and relatively high upper state energies ($\sim$ 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.
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