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Near-Infrared spectra of Jupiters South Equatorial Belt (SEB) with AAT/IRIS2 in H and K bands at a resolving power of R~2400 have been obtained. By creating line-by-line radiative transfer models with the latest improved spectral line data for ammonia and methane (HITRAN2016), we derive best models of cloud/haze parameters in Jupiters South Equatorial Belt. The modelled spectra fit the observations well except for small, isolated discrepancies in the trough region of H2-H2 collision-induced-absorption around 2.08 {mu}m and the methane absorption level between 2.16 and 2.19 {mu}m in K band and at the high pressure methane window between 1.596 to 1.618 {mu}m in H band.
Moist convective storms in Jupiter develop frequently and can trigger atmospheric activity of different scales, from localized storms to planetary-scale disturbances including convective activity confined inside a larger meteorological system. In Feb
The dark colors of Jupiters North Equatorial Belt (NEB, $7-17^circ$N) appeared to expand northward into the neighboring zone in 2015, consistent with a 3-5 year cycle of activity in the NEB.
Mid-infrared 7-20 $mu$m imaging of Jupiter demonstrates that the increased albedo of Jupiters South Equatorial Belt (SEB) during the `fade (whitening) event of 2009-2010 was correlated with changes to atmospheric temperature and aerosol opacity. The
We present revised near-infrared albedo fits of 2835 Main Belt asteroids observed by WISE/NEOWISE over the course of its fully cryogenic survey in 2010. These fits are derived from reflected-light near-infrared images taken simultaneously with therma
Oxygen is the most common element after hydrogen and helium in Jupiters atmosphere, and may have been the primary condensable (as water ice) in the protoplanetary disk. Prior to the Juno mission, in situ measurements of Jupiters water abundance were