VHF volume-imaging radar observation of aspect-sensitive scatterers tilted in mountain waves above a convective boundary layer
Thin stable atmospheric layers cause VHF radars to receive increased echo power from near zenith. Layers can be tilted from horizontal, for instance by gravity waves, and the direction of VHF "glinting" is measurable by spatial domain interferometry or many-beam Doppler beam swinging (DBS). This...
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| Format: | Artigo |
| Sprache: | Inglês |
| Veröffentlicht: |
Copernicus Publications
2005-06-01
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| Schriftenreihe: | Annales Geophysicae |
| Online-Zugang: | https://www.ann-geophys.net/23/1139/2005/angeo-23-1139-2005.pdf |
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