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- W2022044968 abstract "A major tornado spawned by a supercell is reproduced by a fine-resolution three-dimensional numerical simulation, and its genesis mechanism and structure are clarified. The tornado, which is associated with a maximum vertical vorticity of 0.85 s-1 and a pressure drop of 27 hPa, originates from one of the small-scale vortices on the gust front that forms between a warm moist environmental air and a rain-cooled air produced by the storm. Only the small-scale vortex that develops into a major tornado is located right under the low-level updraft associated with the low-level mesocyclone; the others that fail to develop are not. Several interesting previously-unexamined characteristics of the threedimensional structure of the simulated tornado vortex are also reported." @default.
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- W2022044968 date "2005-01-01" @default.
- W2022044968 modified "2023-10-03" @default.
- W2022044968 title "Genesis and Structure of a Major Tornado in a Numerically-Simulated Supercell Storm: Importance of Vertical Vorticity in a Gust Front" @default.
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- W2022044968 doi "https://doi.org/10.2151/sola.2005-002" @default.
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