Some fundamental questions concerning the circulation of the atmosphere of Venus

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Abstract

There has been very little new data on the atmosphere of Venus in recent years, but ongoing studies of data from space missions such as Pioneer Venus, Venera and Galileo, plus ground-based observations, have uncovered, but not yet resolved, a number of fundamental questions relating to the atmospheric global circulation. In addition to the perennial problem of trying to understand the forces driving the equatorial super-rotation, there is still no reliable model, even in the qualitative sense, of the mean meridional (equator-to-pole) circulation, nor of the peculiar giant polar vortices which are a major feature of it. There is pronounced meteorological activity in the upper troposphere, the general character of which, let alone the processes responsible, remains unknown. The very limited observations of temperature and compositional trends, wave motions and cloud features which exist at present provide some clues as to what may be happening on the Earth's twin planet and suggest the next steps towards a more detailed, quantitative understanding.

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    Venus has a very complicated atmospheric dynamical system. The driving force behind the zonal super rotation, the dynamics of the polar vortices, and the meridional circulation as well as the cause of temporal and spatial variations of the cloud layer opacity are all rather poorly understood (Moroz, 2002; Taylor, 2002; Titov et al., 2002). [MO4] Aerosols in the cloud layers

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