An equilibrium statistical theory of coherent structures is applied to midl
atitude bands in the northern and southern hemispheres of Jupiter. The theo
ry imposes energy and circulation constraints on the large-scale motion and
uses a prior distribution on potential vorticity fluctuations to parameter
ize the small-scale turbulent eddies. Nonlinearly stable coherent structure
s are computed by solving the constrained maximum entropy principle governi
ng the equilibrium states of the statistical theory. The theoretical predic
tions are consistent with the observed large-scale features of the weather
layer if and only if the prior distribution has anticyclonic skewness, mean
ing that intense anticyclones predominate at small scales. Then the computa
tions show that anticyclonic vortices emerge at the latitudes of the Great
Red Spot and the White Ovals in the southern band, whereas in the northern
band no vortices form within the zonal jets. Recent observational data from
the Galileo mission support the occurrence of intense small-scale anticycl
onic forcing. The results suggest the possibility of using equilibrium stat
istical theory for inverse modeling of the small-scale characteristics of t
he Jovian atmosphere from observed features.