Note to users. If you're seeing this message, it means that your browser cannot find this page's style/presentation instructions -- or possibly that you are using a browser that does not support current Web standards. Find out more about why this message is appearing, and what you can do to make your experience of our site the best it can be.


Science 8 September 2000:
Vol. 289. no. 5485, pp. 1737 - 1740
DOI:

Reports

Nonlinear Simulations of Jupiter's 5-Micron Hot Spots

Adam P. Showman,1* Timothy E. Dowling2*

Large-scale nonlinear simulations of Jupiter's 5-micron hot spots produce long-lived coherent structures that cause subsidence in local regions, explaining the low cloudiness and the dryness measured by the Galileo probe inside a hot spot. Like observed hot spots, the simulated coherent structures are equatorially confined, have periodic spacing, propagate west relative to the flow, are generally confined to one hemisphere, and have an anticyclonic gyre on their equatorward side. The southern edge of the simulated hot spots develops vertical shear of up to 70 meters per second in the eastward wind, which can explain the results of the Galileo probe Doppler wind experiment.

1 National Research Council (NRC)/NASA Ames Research Center, Mail Stop 245-3, Moffett Field, CA 94035-1000, USA.
2 Comparative Planetology Laboratory, University of Louisville, 211 Sackett Hall, Louisville, KY 40292, USA.
*   E-mail: showman{at}humbabe.arc.nasa.gov (A.P.S.); dowling{at}flolab.spd.louisville.edu (T.E.D.)


Read the Full Text


THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
Oxygen and Other Volatiles in the Giant Planets and their Satellites.
M. H. Wong, J. I. Lunine, S. K. Atreya, T. Johnson, P. R. Mahaffy, T. C. Owen, and T. Encrenaz (2008)
Reviews in Mineralogy and Geochemistry 68, 219-246
   Abstract »    Full Text »    PDF »



To Advertise     Find Products


Science. ISSN 0036-8075 (print), 1095-9203 (online)