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
Cite
CITATION STYLE
Weisman, M. L., & Klemp, J. B. (1984). The structure and classification of numerically simulated convective storms in directionally varying wind shears. Monthly Weather Review, 112(12), 2479–2498. https://doi.org/10.1175/1520-0493(1984)112<2479:TSACON>2.0.CO;2
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