110 citations · 193 across the 6 of their papers we have counts for
8 papers
Referencing Sources of Molecular Spectroscopic Data in the Era of Data Science: Application to the HITRAN and AMBDAS Databases
Frances M. Skinner, Iouli E. Gordon, Christian Hill +3
The application described has been designed to create bibliographic entries in large databases with diverse sources automatically, which reduces both the frequency of mistakes and…
Empirical normal intensity distribution for overtone vibrational spectra of triatomic molecules
Emile S. Medvedev, Vladimir G. Ushakov, Eamon K. Conway +3
Theoretical calculations are contributing a significantly higher proportion of data to contemporary spectroscopic databases, which have traditionally relied on experimental observa…
Calculated line lists for HO and HO with extensive comparisons to theoretical and experimental sources including the HITRAN2016 database
Eamon K. Conway, Iouli E. Gordon, Aleksandra A. Kyuberis +3
New line lists are presented for the two most abundant water isotopologues; HO and HO. The HO line list extends to 25710 cm with inten…
An accurate, extensive, and practical line list of methane for the HITEMP database
Robert J. Hargreaves, Iouli E. Gordon, Michael Rey +4
A methane line list for the HITEMP spectroscopic database, covering 0-13,400 cm (746 nm), is presented. To create this compilation, ab initio line lists of CH$_{4}…
Use of the complete basis set limit for computing highly accurate ab initio dipole moments
Eamon K. Conway, Iouli E. Gordon, Oleg L. Polyansky +1
Calculating dipole moments with high-order basis sets is generally only possible for the light molecules, such as water. A simple, yet highly effective strategy of obtaining high-o…
Introduction of water-vapor broadening coefficients and their temperature dependence exponents into the HITRAN database, Part I: CO2, N2O, CO, CH4, O2, NH3, and H2S
Yan Tan, Roman V. Kochanov, Laurence S. Rothman +1
The amount of water vapor in the terrestrial atmosphere is highly variable both spatially and temporally. In the tropics it sometimes constitutes 4-5% of the atmosphere. At the sam…