Journal
ASTROPHYSICAL JOURNAL SUPPLEMENT SERIES
Volume 235, Issue 1, Pages -Publisher
IOP PUBLISHING LTD
DOI: 10.3847/1538-4365/aaa07a
Keywords
molecular data; planets and satellites: atmospheres; planets and satellites: gaseous planets; radiative transfer; techniques: spectroscopic
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Funding
- Royal Society Research Fellowship
- European Research Council Consolidator Grant (under the European Union's Horizon 2020 research and innovation programme) at the University of Leicester [723890]
- Knut and Alice Wallenberg Foundation
- National Aeronautics and Space Administration
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Despite being one of the weakest dimers in nature, low-spectral-resolution Voyager/IRIS observations revealed the presence of (H-2)(2) dimers on Jupiter and Saturn in the 1980s. However, the collision-induced H-2-H-2 opacity databases widely used in planetary science have thus far only included free-to-free transitions and have neglected the contributions of dimers. Dimer spectra have both fine-scale structure near the S(0) and S(1) quadrupole lines (354 and 587 cm(-1), respectively), and broad continuum absorption contributions up to +/- 50 cm(-1) from the line centers. We develop a new ab initio model for the free-to-bound, bound-to-free, and bound-to-bound transitions of the hydrogen dimer for a range of temperatures (40-400 K) and para-hydrogen fractions (0.25-1.0). The model is validated against low-temperature laboratory experiments, and used to simulate the spectra of the giant planets. The new collision-induced opacity database permits high-resolution (0.5-1.0 cm(-1)) spectral modeling of dimer spectra near S(0) and S(1) in both Cassini Composite Infrared Spectrometer observations of Jupiter and Saturn, and in Spitzer Infrared Spectrometer (IRS) observations of Uranus and Neptune for the first time. Furthermore, the model reproduces the dimer signatures observed in Voyager/IRIS data near S(0) on Jupiter and Saturn, and generally lowers the amount of para-H-2 (and the extent of disequilibrium) required to reproduce IRIS observations.
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