Abstract
Using a three-dimensional numerical cloud model, we investigate the effects of directionally varying wind shear on convective storm structure and evolution over a wide range of shear magnitudes. As with a previous series of experiments using unidirectional wind shear profiles, the current results evince a spectrum of storm types ranging from short lived single cells at low shears, multicells at intermediate shears, to supercells at high shears. With a clockwise curved hodograph, the supercellular growth is confined to the right flank of the storm system while multicellular growth is favored on the left flank. -from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 2479-2498 |
| Number of pages | 20 |
| Journal | Monthly Weather Review |
| Volume | 112 |
| Issue number | 12 |
| DOIs | |
| State | Published - 1984 |
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