Teleconvection: Remotely Driven Thermal Convection in Rotating Stratified Spherical Layers
Keke Zhang,*
Gerald Schubert
We report the discovery of a convective phenomenon found
to occur in a rotating spherical system in which an inner convectively unstable fluid layer is bounded by a corotating outer convectively stable fluid layer. Although convection is thermally driven in the
unstable interior, the resulting convective motions concentrate primarily in the stable outer region. This phenomenon, which we term
teleconvection, suggests that fluid motions observed at the "surface" of a planet (such as Jupiter's alternating zonal winds) may be driven by an energy source located deep inside the planet.
Department of Earth and Space Sciences and Institute of Geophysics
and Planetary Physics, University of California, Los Angeles, CA 90095, USA.
*
Present address: School of Mathematical Sciences, University of
Exeter, Exeter EX4 4QE, UK.
To whom correspondence should be addressed.