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- W2012330900 abstract "Abstract A three-dimensional numerical simulation of an intense, quasi-steady left-moving thunderstorm observed over mountainous terrain is presented. The observational analysis of the evolution of convection leading to this storm is presented in Part I, and a detailed analysis of the Doppler radar-observed storm structure is presented in Parts II and III. This storm was particularly interesting because it initially grew in an environment characterized by terrain-induced boundary layer convergence before a massive mesoscale cold front passed underneath. The front cooled and moistened low levels while veering the surface winds to the north, creating a hodograph of winds strongly backing with height. After frontal passage the initial storm cell grew explosively and turned to the left. The observed storm evolution after the frontal passage was reproduced well by the numerical simulation. An observed secondary updraft which was not simulated, was attributed to residual effects of the prefrontal environment, w..." @default.
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- W2012330900 date "1986-05-01" @default.
- W2012330900 modified "2023-10-18" @default.
- W2012330900 title "An Intense, Quasi-Steady Thunderstorm over Mountainous Terrain. Part IV: Three-Dimensional Numerical Simulation" @default.
- W2012330900 doi "https://doi.org/10.1175/1520-0469(1986)043<0894:aiqsto>2.0.co;2" @default.
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