Observation of Kelvin-Helmholtz and propagating buoyancy waves in the Antarctic with the help of sodar and microbarograph
Internal gravity waves of different types are frequently observed in the stable atmoshperic boundary layer. The most common way to study the waves is analysis of pressure records. Remote sensing techniques also can be used to observe the waves and to estimate their parameters. We used synchronous so...
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Veröffentlicht in: | IOP conference series. Earth and environmental science 2019-02, Vol.231 (1), p.12054 |
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Format: | Artikel |
Sprache: | eng |
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