Rainfall evaporation in thunderstorm downdraughts
It is explained that in air descending at speeds of some m sec−1 raindrop evaporation must proceed at a large subsaturation. Under some simplifying steady‐state assumptions, the vertical temperature profiles in thunderstorm downdraughts of a range of speeds are estimated, and it is shown that the mo...
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| Veröffentlicht in: | Quarterly journal of the Royal Meteorological Society 1966-10, Vol.92 (394), p.510-518 |
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| Hauptverfasser: | , |
| Format: | Artikel |
| Sprache: | eng |
| Online-Zugang: | Volltext |
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