Takemi (2007) の設定における二次元計算 (温度: 熱帯場, 湿度: Q18, 2.5 km～5.0 km に鉛直シアーのある風, Us = 15 ms^-1)

概要

図の破線 (Takemi, 2007)
- 風のシアーを与える高度
  - 2.5 - 5.0 km
- 風のシアー中の最大風速 (Us)
  - U_s = 15 m/s

Takemi, T., 2007: A sensitivity of squall-line intensity to environmental static stability under various shear and moisture conditions Atmospheric Research Volume 84, Issue 4, June 2007, Pages 374-389
Takemi, T., 2006: Impacts of moisture profiles on the evolution and organization of midlatitde squall lines under various shear conditions, Atmos. Res., Vol.82.
Weisman, M.L., Klemp, J.B., 1982. The dependence of numerically simulated convective storms on vertical wind shear and buoyancy. Mon. Weather Rev. 110, 504-520.

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