Astronomy and Astrophysics – Astronomy
Scientific paper
Oct 2010
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2010dps....42.3106s&link_type=abstract
American Astronomical Society, DPS meeting #42, #31.06; Bulletin of the American Astronomical Society, Vol. 42, p.1010
Astronomy and Astrophysics
Astronomy
Scientific paper
A prominent characteristic of Jovian near-IR spectra is the widely distributed presence of a strong absorption at 2.9-3.1 microns, first noticed in a 3-micron spectrum obtained by the Infrared Space Observatory (ISO) in 1996. While Brooke et al. (1998, Icarus 136, 1-13) were able to fit the ISO spectrum using ammonia ice as the sole source of particulate absorption, Irwin et al. (2001, Icarus 149, 397-415) noted that their best-fit cloud model implied a strong absorption at 2 microns that was not observed in Galileo NIMS spectra. Subsequent significant revisions in ammonia gas absorption models (Bowles et al. 2008, Icarus 196, 612-614) also raised questions about the Brooke et al. results because ammonia gas absorption overlaps regions of ammonia ice absorption. Our reanalysis, based on improved ammonia absorption models, finds that the ISO spectrum can be fit much better with NH4SH as the sole 3-micron absorber than with NH3. But even better fits result from cloud models that include both NH3 ice and NH4SH, with the latter substance providing most of the absorption. The component due to NH3 is very possibly in the form of a coating on either large (r 15 microns) particles in a deeper layer at 550 mb or on small (r 0.3 micron) photochemical haze particles in a higher layer near 370 mb. Neither option conflicts with the lack of significant NH3 absorption features at thermal wavelengths. VIMS spectral fits (Sromovsky and Fry 2010, Icarus in press, doi:10.1016/j.icarus.2010.06.039) are also compatible with NH4SH as the primary 3-micron absorber, and also benefit from the inclusion of a layer of small (r 0.3 micron) composite particles, with NH3 as a minor fraction, either as coating or core.
This work was supported by NASA Outer Planets Research Program, the Cassini Data Analysis program, and the Jupiter Data Analysis Program.
Fry Patrick M.
Sromovsky Lawrence A.
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