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• W1966973616 abstract "Turbulence is important for its effects on atmospheric chemistry, mixing air of different composition. For over 40 years, it has been known that wind shear associated with the jet stream is one important cause. However, atmospheric radar shows that other processes are also very significant—specifically, the breaking of internal gravity-waves generated by flow of air over mountains. These mountain waves propagate upward from their source near the ground, and can generate turbulence many kilometres higher in the atmosphere. Turbulence near the tropopause level has been invoked as a mechanism for exchange of air between stratosphere and troposphere, including constituents such as ozone and water vapour. VHF radar data here show direct, high-resolution evidence of this turbulence, persisting for two days. Breaking of mountain waves is known to be an essential input for improved global circulation models and weather models; also, on a more general note, atmospheric turbulence at these altitudes is not only an abstract problem, but experienced at first hand through its dangerous effect on jet aircraft travel. Calculations of the intensity of turbulence, using energy dissipation rates derived from broadening of Doppler echo spectra, show that mountain wave breaking is sometimes the single most important source of turbulence in the lower atmosphere." @default.
• W1966973616 created "2016-06-24" @default.
• W1966973616 creator A5087250738 @default.
• W1966973616 date "1998-11-01" @default.
• W1966973616 modified "2023-10-16" @default.
• W1966973616 title "Tropopausal turbulence caused by the breaking of mountain waves" @default.
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• W1966973616 doi "https://doi.org/10.1016/s1364-6826(98)00105-9" @default.
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