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Solar System Observations with ISO

Emmanuel Lellouch 

Observatoire de Paris, Meudon, France




The ISO observations of Solar System objects have been crown with considerable success. The amount, quality and diversity of the results exceeds most expectations. This success is due, in a large part, to the outstanding performances of the SWS instrument, and to the close cooperation between the SWS team and Solar System Mission Scientist T. Encrenaz and her team. The lucky appearance of comet Hale-Bopp during the lifetime of the mission was another factor. The results cover a variety of areas: (1) the formation of Giant Planets (2) the physics and composition of planetary atmospheres and environments (3) the composition and thermal properties of planetary, satellite and asteroid surfaces (4) the composition of cometary atmospheres, ices and dust and their implications for cometary activity and formation (5) the composition and properties of interplanetary dust. This talk will highlight the most important results known to the author at that time. As an appetizer: ISO has allowed the first detection of (i) the far-IR lines of HD in the four Giant Planets, allowing a coherent determination of their D/H ratio (ii) water vapor in the upper atmosphere of the four Giant Planets and Titan, implying the existence of an external source of oxygen in these objects, probably linked to interplanetary dust particles (iii) new hydrocarbon species of the Giant Planets, notably CH3, C6H6, C3H4 and C4H2 in Saturn, with implications for the chemistry and vertical transport in their stratospheres (iv) the spectral signature of NH3 clouds in Jupiter's atmosphere (v) a low, undersaturated, abundance of water in Saturn's upper troposphere (vi) the presence of crystalline silicates in a short-period comet (P/Hartley 2), and of Mg-rich crystalline silicates (forsterite) in Oort-cloud comet Hale-Bopp (vii) the abundant presence of CO2 in these two comets. Other results non-exhaustively include an indication for the long-sought presence of carbonates on Mars, the first observation of a thermal lightcurve for Pluto and the evidence for narrow features near 10 $\mu$m in the spectrum of Vesta.


next up previous contents index
Next: Oxygen in the stratospheres Up: ORAL TALKS (by order Previous: ISOPHOT - Performance, Results
"The Universe as seen by ISO", 20 - 23 October 1998, Paris: Abstract Book