Evaluation of a technique for radar identification of large hail across the upper midwest and central plains of the United States
Radar data were analyzed for severe thunderstorms that produced severe hail (>19 mm diameter) across the central and northern plains of the United States during the 2001–04 convective seasons. Results showed a strongly linear relationship between the 50-dBZ echo height and the height of the melti...
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Veröffentlicht in: | Weather and forecasting 2007-04, Vol.22 (2), p.244-254 |
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