Venus zonal wind above the cloud layer |
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Authors: | RS Lindzen H Teitelbaum |
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Institution: | 1. Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, Massachusetts 02139, USA;2. Laboratoire de Métérologie Dynamique du CNRS, Ecole Polytechnique, 91128 Palaiseau Cedex, France |
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Abstract: | The altitude variation of the zonal wind velocity in the Venus atmosphere above the cloud layer is deduced from the structure of the wavenumber 2 solar tide. Results show that the amplitude of the zonal wind increases with respect to altitude near the equator, but decreases for latitudes greater than 30°. Thus, the zonal wind becomes concentrated at lower latitudes by 100 km altitude. |
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