Presentation #102.22 in the session Poster Session.
The HITRAN2020 edition includes newly added or updated planetary broadening parameters applicable to modeling and interpreting spectra of planetary and exoplanetary atmospheres . These new parameters include broadening due to ambient pressure of H2O , He, H2, and CO2 . Planetary broadeners were first added to the database during the HITRAN2016 edition for the line lists of; SO2, NH3, HF, HCl, OCS, and C2H2 . Since then, He, H2, and CO2 broadening parameters, as well as their temperature dependencies, and in some cases, pressure-induced shifts have been added and/or updated for the line lists of; CO2, N2O, CO, SO2, OH, OCS, H2CO, HCN, PH3, H2S, and GeH4 . By using these planetary broadeners, in conjunction with the HITRAN Application Programming Interface (HAPI) , a reliable planetary reference opacity can be calculated. As a test case, this work investigates how the HITRAN broadening data can be used to model spectra under Jovian and Venusian conditions, with resultant opacities compared to available laboratory data [6–9]. Specifically, opacities of NH3 broadened by H2, He, and H2O are tested against laboratory data that are utilized by the Juno mission to retrieve atmospheric molecular constituents of Jupiter [10, 11]. In addition, due to the recent tentative detection of PH3 on Venus  and subsequent studies regarding correlation of the signal with lines of SO2 [13, 14], the opacities of PH3 and SO2 under Venusian conditions are also modeled. Overall, this work demonstrates how HITRAN and HAPI along with the newly included planetary broadeners can be utilized to generate opacities under diverse planetary conditions.
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