HR: 14:25h
AN: P23C-04 INVITED [Abstracts]
TI: Eddies, Convection, and Maintenance of the Saturn General Circulation: Results from Cassini
Imaging
AU: * Del Genio, A D
EM: adelgenio@giss.nasa.gov
AF: NASA/GISS, 2880 Broadway, New York, NY 10025-7848, United States
AU: Barbara, J M
EM: jbarbara@giss.nasa.gov
AF: Sigma Space Partners, LLC, Institute for Space Studies
2880 Broadway, New York, NY 10025-7848, United States
AU: Ferrier, J
EM: jferrier@giss.nasa.gov
AF: Sigma Space Partners, LLC, Institute for Space Studies
2880 Broadway, New York, NY 10025-7848, United States
AU: Ingersoll, A P
EM: api@gps.caltech.edu
AF: California Institute of Technology, Division of Geological and Planetary Sciences, 150-21,
Pasadena, CA 91125, United States
AU: West, R A
EM: Robert.A.West@jpl.nasa.gov
AF: Jet Propulsion Laboratory, Caltech, 4800 Oak Grove Drive, Pasadena, CA 91109, United
States
AU: Vasavada, A R
EM: ashwin.r.vasavada@jpl.nasa.gov
AF: Jet Propulsion Laboratory, Caltech, 4800 Oak Grove Drive, Pasadena, CA 91109, United
States
AU: Spitale, J
EM: spitale@jupiter.lpl.arizona.edu
AF: Cassii Imaging Central Laboratory for Operations, Space Science Institute
4750 Walnut Street, Suite 205, Boulder, CO 80301, United States
AU: Porco, C
EM: carolyn@ciclops.org
AF: Cassii Imaging Central Laboratory for Operations, Space Science Institute
4750 Walnut Street, Suite 205, Boulder, CO 80301, United States
AB:
Cassini ISS imaging of Saturn's southern hemisphere during approach and in the months after orbit insertion
have shown the mean zonal wind pattern to be relatively invariant with time outside the equatorial region. A major
objective of the Cassini imaging investigation is to deduce the physical processes responsible for maintaining
the momentum balance of the Saturn jets and to thereby constrain theories of jovian planet circulation. A related
question is whether the mean meridional overturning circulation on Saturn more closely resembles Earth's
tropical Hadley cell, with convective heating driving a thermally direct circulation, or its midlatitude Ferrel cell, with
larger-scale eddies mechanically driving a thermally indirect overturning. Voyager images provided too small a
sample at too low resolution to address this issue. For Cassini, we applied an automated cloud tracking
algorithm to pairs of images over 4 Saturn rotations to estimate eddy fluxes of zonal momentum. The resulting
dataset produces an order of magnitude more wind vectors than were the case for Voyager, with relatively
unbiased sampling. The results show clear patterns of eddy momentum flux that are positively correlated with
the latitudinal shear of the mean zonal wind, indicating that eddies are supplying the kinetic energy of the mean
flow. We also detect moist convective storms by monitoring the evolution of anomalous bright features in
continuum images, with supporting evidence of high cloud tops in weak methane band images when available.
These show a tendency for convection to occur preferentially in cyclonic shear zones and not at all in anti-cyclonic
shear regions. This implies that air rises in the cyclonic regions, drifts equatorward (poleward) across eastward
(westward) jets, and sinks in the anti-cyclonic regions. The Coriolis force on the implied mean meridional flow
decelerates (accelerates) these jets, potentially balancing the acceleration (deceleration) due to the eddy fluxes.
This picture is consistent with recent Cassini and Galileo inferences about Jupiter and supports the Ferrel cell
picture. Recent models that simulate baroclinic instability on jovian planets produce similar momentum
balances. Latent heating due to moist convection in this picture may create the temperature contrasts that drive
the baroclinic eddies that perform most of the eddy momentum transport. Recent images providing our first look
at Saturn's northern hemisphere during the Cassini era show that the westward (eastward) jets at 34 (42)
degrees North planetocentric latitude are still present, and that eddy fluxes are positively correlated with the mean
zonal wind shear for this jet pair as well.
DE: 3346 Planetary meteorology (5445, 5739)
DE: 3360 Remote sensing
DE: 5445 Meteorology (3346)
DE: 5704 Atmospheres (0343, 1060)
DE: 5739 Meteorology (3346)
SC: Planetary Sciences [P]
MN: 2007 Fall Meeting