Integration of radar with analysis fields — Bringing distant radar observations “down to earth”
Normal refraction of radar waves through the atmosphere prevents radar data at distant ranges from being quantitatively representative for the Earth's surface unless precipitation-related processes taking place between the radar echo and the surface are taken into account. A one-dimensional mod...
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Veröffentlicht in: | Physics and chemistry of the earth. Part B, Hydrology, oceans and atmosphere Hydrology, oceans and atmosphere, 2000, Vol.25 (10-12), p.1033-1036 |
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Format: | Artikel |
Sprache: | eng |
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