1. INTRODUCTION
The weather on Jupiter appears to be stormy in most of the time. Lightning flashes deep in the enveloping gas clouds
and eddies of atmospheric turbulence bob along the margins of jet streams while the thunderheads tower about 50 km
above surrounding clouds. Observations show that moist heat rising in these stormy updrafts supplies the required
energy responsible for forming the Jupiter weather [1]. Analyzing photographs obtained from the Galileo spacecraft,
orbiting the planet, it has been reported that this moist convection of thunderstorms on Jupiter is to some extent similar
to that on Earth but is produced by heat from deep in the planet and not from sunlight as in Earth. Many scientists are
confused to solve the mystery of how Jupiter gets the energy for a constantly stormy weather system. A team of
astronomers led by Gierasch [2] obtained the evidence of a permanent storm in the southern hemisphere by considering
the images from visible and infrared light. Lightning was visible initially and thereafter a cluster of Earthlike storms
were developed there. Astronomers estimated that the vertical transport of heat generated by such storms corresponded
to the flux produced by the planet's internal heat source. In this paper the cloud pattern at different Jupiter belts and the
vertical structure of its atmosphere are examined and the elemental abundances relative to hydrogen for Sun as well as
Jupiter to Sun have been taken into account including the unique characteristics of belts and zones. Jupiter's Little Red
Spot has been considered as the precursor of storms and the properties of vortices formed in Jupiter are examined
pointing out mystery of some related observations.