The deuterium abundance in Jupiter and Saturn from ISO-SWS observations
By E. Lellouch, B. Bézard, T. Fouchet, H. Feuchtgruber, T. Encrenaz, T. Graauw. 2001
211 citations recorded by the source corpus.
Subfields: Astronomy and Astrophysics, Atmospheric Science, Spectroscopy
View Paper: https://www.semanticscholar.org/paper/b3da823f73b0afdd4bd24a8c37175c7b85f0cc20
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Citations in the corpus
- Photochemistry and diffusion in Jupiter's stratosphere: Constraints from ISO observations and comparisons with other giant planets (2005, methodology): “, 2000; Lellouch et al., 2002; Kunde et al., 2004]. Therefore global-average and 1-D models of oxygen compounds are not very meaningful for Jupiter in the post-SL9 era. Lellouch et al. [2002] provide model-data comparisons that suggest that H2O and CO2 originate from the deposition of oxygen compoun”
- Origin of water in the terrestrial planets (2005, background): “The D/H ratio of the nebular gas is inferred from spectroscopic measurements of CH4 in the atmospheres of Jupiter and Saturn to be 2.1 ± 0.4 × 10−5 (Lellouch et al. 2001), much lower than VSMOW.”
- The chemical composition of the Sun (2009, methodology): “Using ISO spectra of the Jovian atmosphere and taking into account an expected 5−10% enrichment during the planet’s formation, Lellouch et al. (2001) obtained a proto-solar abundance of D/H = (2.1 ± 0.4) · 10−5.”
- What Is the Total Deuterium Abundance in the Local Galactic Disk? (2006, background): “Analysis of Infrared Space Observatory (ISO) spectra of H2, HD, CH4, and CH3D in Jupiter’s atmosphere led Lellouch et al. (2001) to infer (D/H)psc = 21 ± 4 ppm, although there are many assumptions that go into this analysis.”
- The composition of Titan's stratosphere from Cassini/CIRS mid-infrared spectra (2007, background): “This potential problem was noted in ISO observations of Saturn (Lellouch et al., 2001).”