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Scientific and Technical Aerospace Reports Volume 38 July 28, 2000

Scientific and Technical Aerospace Reports Volume 38 July 28, 2000

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<strong>2000</strong>0064708 Jet Propulsion Lab., California Inst. of Tech., Pasadena, CA USA<br />

Photochemistry of Saturn’s Atmosphere, 1, Hydrocarbon Chemistry <strong>and</strong> Comparisons with ISO Observations<br />

Moses, Julianne I., Lunar <strong>and</strong> Planetary Inst., USA; Bezard, Bruno, Observatoire de Paris-Meudon, France; Lellouch, Emmanuel,<br />

Observatoire de Paris-Meudon, France; Gladstone, G. R<strong>and</strong>all, Southwest Research Inst., USA; Feuchtgruber, Helmut, Max-<br />

Planck-Inst. fuer Extraterrestrische Physik, Germany; Allen, Mark, Jet Propulsion Lab., California Inst. of Tech., USA; Icarus;<br />

<strong>2000</strong>; ISSN 0019-1035; <strong>Volume</strong> I43, pp. 244-298; In English<br />

Contract(s)/Grant(s): NASw-4574; NAG5-6915<br />

Report No.(s): LPI-Contrib-982; Copyright; Avail: Issuing Activity<br />

To investigate the details of hydrocarbon photochemistry on Saturn, we have developed a one-dimensional diurnally averaged<br />

model that couples hydrocarbon <strong>and</strong> oxygen photochemistry, molecular <strong>and</strong> eddy diffusion, radiative transfer, <strong>and</strong> condensation.<br />

The model results are compared with observations from the Infrared Space Observatory (ISO) to place tighter constraints<br />

on molecular abundances, to better define Saturn’s eddy diffusion coefficient profile, <strong>and</strong> to identify important chemical schemes<br />

that control the abundances of the observable hydrocarbons in Saturn’s upper atmosphere. From the ISO observations, we determine<br />

that the column 12 densities of CH3, CH3C2H, <strong>and</strong> C4H2 above 10 mbar are 4 (sup +2) (sub -1.5) x 10 (exp 13) cm (sup<br />

-2), (1.1 plus or minus 0.3) x 10 (exp 15) cm (exp -2), <strong>and</strong> (1.2 plus or minus 0.3) x 10 (exp 14) cm (sup -2), respectively. The<br />

observed ISO emission features also indicate C2H2 mixing ratios of 1.2 (sup +0.9) (sub -0.6) x 10 (exp -6) at 0.3 mbar <strong>and</strong> (2.7<br />

plus or minus 0.8) x 10 (exp -7) at 1.4 mbar, <strong>and</strong> a C2H6 mixing ratio of (9 plus or minus 2.5) x 10 (exp -6) at 0.5 mbar. Upper<br />

limits are provided for C2H4, CH2CCH2, C3H8, <strong>and</strong> C6H2 sensitivity of the model results to variations in the eddy diffusion<br />

coefficient profile, the solar flux, the CH4 photolysis branching ratios, the atomic hydrogen influx, <strong>and</strong> key reaction rates are discussed<br />

in detail. We find that C4H2 <strong>and</strong> CH3C2H are particularly good tracers of important chemical processes <strong>and</strong> physical conditions<br />

in Saturn’s upper atmosphere, <strong>and</strong> C2H6 is a good tracer of the eddy diffusion coefficient in Saturn’s lower stratosphere.<br />

The eddy diffusion coefficient must be smaller than approximately 3 x 10 (exp 4) sq cm s (sup -1) at pressures greater than 1 mbar<br />

in order to reproduce the C2H6 abundance inferred from ISO observations. The eddy diffusion coefficients in the upper stratosphere<br />

could be constrained by observations of CH3 radicals if the low-temperature chemistry of CH3 were better understood.<br />

We also discuss the implications of our modeling for aerosol formation in Saturn’s lower stratosphere-diacetylene, butane, <strong>and</strong><br />

water condense between approximately 1 <strong>and</strong> 300 mbar in our model <strong>and</strong> will dominate stratospheric haze formation at nonauroral<br />

latitudes. Our photochemical models will be useful for planning observational sequences <strong>and</strong> for analyzing data from the upcoming<br />

Cassini mission.<br />

Author<br />

Saturn (Planet); Saturn Atmosphere; Photochemical Reactions; Upper Atmosphere; Infrared Astronomy; Mathematical Models<br />

<strong>2000</strong>0064716 NASA Kennedy Space Center, Cocoa Beach, FL USA<br />

Titan III Mars Observer Press Showing at the PHSF<br />

Aug. 13, 1992; In English; Videotape: 2 min. 30 sec. playing time, in color, no sound<br />

Report No.(s): NONP-NASA-VT-<strong>2000</strong>081554; No Copyright; Avail: CASI; B01, Videotape-Beta; V01, Videotape-VHS<br />

Live footage of the Titan 3 Mars Observer is shown at the Payload Hazardous Servicing Facility (PHSF). The Mars Observer<br />

is a NASA mission to study the surface, atmosphere, interior <strong>and</strong> magnetic field of Mars from Martian orbit.<br />

CASI<br />

Mars Observer; Payloads; Titan 3 Launch Vehicle<br />

<strong>2000</strong>0065630 NASA Kennedy Space Center, Cocoa Beach, FL USA<br />

Mars Observer Press Conference<br />

Aug. 25, 1993; In English; Videotape: 18 min. 5 sec. playing time, in color, with sound<br />

Report No.(s): NONP-NASA-VT-<strong>2000</strong>081551; No Copyright; Avail: CASI; B02, Videotape-Beta; V02, Videotape-VHS<br />

Footage shows Bob MacMillin, NASA’s Public Information Office, as he introduces the Mars Observer Project Manager,<br />

Glen Cunningham. Glen is shown addressing the current status of the Mars Observer communication system, the inability of<br />

NASA to establish contact, <strong>and</strong> the action that is currently being taken to establish contact with the spacecraft. Glen is also seen<br />

answering questions from both the audience as well as other NASA Centers.<br />

CASI<br />

Conferences; Mars Observer<br />

230

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