Effects of the Low-Level Wind Profile on Outflow Position and Near-Surface Vertical Vorticity in Simulated Supercell Thunderstorms
Effects of the Low-Level Wind Profile on Outflow Position and Near-Surface Vertical Vorticity in Simulated Supercell Thunderstorms
复制标题
模拟超级单体雷暴中低空风廓线对流出位置和近地表垂直涡度的影响
DOI:
10.1175/jas-d-17-0174.1
复制
发表时间:
2018
影响因子:
3.1
通讯作者:
Epifanio, Craig C.
中科院分区:
文献类型:
--
作者:
Guarriello, Felicia;Nowotarski, Christopher J.;Epifanio, Craig C.
Supercell thunderstorms are simulated using an idealized numerical model to analyze the effects of modifications to the environmental low-level wind profile on near-surface rotation. Specifically, the orientation, magnitude, and depth of the low-level vertical wind shear are modified in several suites of experiments and compared to control simulations with no vertical wind shear in the prescribed layer.The overall morphology of the simulated supercells is highly sensitive to even shallow changes in the low-level wind profile. Moreover, maximum near-surface vertical vorticity varies as the low-level wind profile is modified. The results suggest this is principally a consequence of the degree to which favorable dynamic forcing of negatively buoyant outflow is superimposed upon the near-surface circulation maximum. Simulations with easterly shear and weaker storm-relative winds over the depth of the gust front promote forward-surging outflow and smaller separation between the near-surface circulation maximum and the mesocyclone aloft compared with other hodograph shapes. This promotes near-surface vertical vorticity intensification in these simulations. Similar trends in near-surface vertical vorticity as a function of low-level shear orientation are observed for varying shear-layer depths and bulk-shear magnitudes over the shear layer. The degree to which specific hodograph shapes promote strong near-surface rotation may vary with different deep-layer wind profiles or thermodynamic environments from those simulated here; however, this study concludes that favorable positioning of the near-surface circulation maximum and mesocyclone aloft are a necessary condition for supercell tornadogenesis and this positioning may be modulated by the low-level wind profile.
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DOI:
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发表时间:
2002
期刊:
--
影响因子:
--
作者:
J. Craven;H. Brooks;J. Hart
通讯作者:
J. Craven;H. Brooks;J. Hart
影响因子:
3.2
作者:
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影响因子:
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作者:
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P. Skinner;C. Weiss;Michael M. French;H. Bluestein;P. Markowski;Yvette P. Richardson
DOI:
--
发表时间:
2007
期刊:
影响因子:
--
作者:
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通讯作者:
M. Xue