A case study of nonmesocyclone Tornado development in northeast Colorado: similarities to waterspout formation
The evolution of the July 26, 1985, Erie, CO., tornado is described by using data from NCAR's CP-2 Doppler radar. This tornado develops within 20 km of the radar site under weakly forced synoptic conditions and weak tropospheric flow, and is not accompanied by a mesocyclone. The initial circula...
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Veröffentlicht in: | Monthly weather review 1989-04, Vol.117 (4), p.843-856 |
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Hauptverfasser: | , |
Format: | Artikel |
Sprache: | eng |
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Online-Zugang: | Volltext |
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