HR: 17:00h
AN: P44A-05 INVITED [Abstracts]
TI: The Saturn Atmosphere: An Early Cassini ISS Perspective
AU: * West, R
EM: robert.a.west@jpl.nasa.gov
AF: Jet Propulsion Lab, Caltech, MS 169-237
4800 Oak Grove Drive, Pasadena, CA 91109
United States
AU: Ingersoll, A
EM: api@gps.caltech.edu
AF: California Institute of Technology, Geological and Planetary Sciences, Pasadena, CA 91125
United States
AU: Del Genio, A
EM: delgenio@giss.nasa.gov
AF: Goddard Institute for Space Studies, 2880 Broadway, New York, NY 10025
United States
AU: Vasavada, A
EM: Ashwin.R.Vasavada@jpl.nasa.gov
AF: Jet Propulsion Lab, Caltech, MS 169-237
4800 Oak Grove Drive, Pasadena, CA 91109
United States
AU: Barbara, J
EM: jbarbara@giss.nasa.gov
AF: Goddard Institute for Space Studies, 2880 Broadway, New York, NY 10025
United States
AU: Porco, C
EM: Carolyn@ciclops.org
AF: Space Science Institute, 4750 Walnut, Suite 205, Boulder, CO 80301
United States
AU: Imaging Team, C
AF: Various, Various, Various, NY 90000
United States
AB:
During the approach and early part of the Cassini tour of the Saturn system the Imaging Science Subsystem (ISS) obtained a
large number of images of Saturn. At this early phase of the mission we report quantitative results for some of the ISS
atmospheric science objectives. Positional measurements of small spots show the same zonal wind profile reported from
Voyager investigations (data from 1980-81) at latitudes outside of +- 18 degrees. In the latitude range within +- 18 degrees
most of the Cassini measurements cluster around 270 m/s (Eastward), whereas the Voyager results are higher (300-470 m/s).
The lower ISS values agree with values reported by Sanches-LaVega et al. (Nature 2003, 423, 623-625) measured from Hubble
Space Telescope images between 1994 and 2002. A few of the Cassini measurements within this latitude band give speeds in the
range 350-390 m/s which overlap (in latitude) the other points with lower values. Latitudinal temperature gradients point
to a decrease in wind with height so some or all of the differences might be interpreted as differences in pressure levels of
the cloud features used to track winds, with the Voyager measurements sensing the deepest. Two large storms in 1990 and
1995 put clouds at higher altitudes in the HST and Cassini epochs. Cloud height models from images in methane bands will be
used to assess this hypothesis. We also observed spot interactions. The westward-moving jet at approximately 36 degrees
south (the one closest to the equator in the southern hemisphere) was particularly active. It had many counter-clockwise
rotating spots, which merged and divided during a few months of observation. A combination of polarization images from the
violet to the near-infrared, methane-band images and ultraviolet images show a complex latitudinal behavior for cloud and
haze structure and haze properties at high southern latitudes.
DE: 5700 PLANETOLOGY: FLUID PLANETS
DE: 5707 Atmospheres--structure and dynamics
SC: Planetary Sciences [P]
MN: 2004 AGU Fall Meeting