Equatorial Jets in Planetary Atmospheres

Physics

Scientific paper

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Scientific paper

THERMAL convection on a global scale in the lower atmosphere of Jupiter redistributes angular momentum so as to produce a well defined westerly jet at high level astride the equator1-3, with a latitudinal width which can be accounted for in terms of quite elementary theoretical ideas1. Available observations are consistent with a similar phenomenon on Saturn1,4. On Earth, equatorial jets are found in the lower stratosphere and in the oceans.

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