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WRFによる竜巻地表近傍風の特性に関する研究

机译:WRF研究龙卷风表面附近风的特征

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The F3 supercell tornado hit Tsukuba City in eastern Japan is one of most destructive tornado ever recorded in Japan which caused one fatality and great property damage. To explore the wind characteristics of tornado in realistic condition, the Weather Research and Forecasting Model (WRF) model has been employed and successfully regenerates this tornado process. Simulation by WRF model is conducted by triply nested domains downscaling horizontal grid resolution from 1 kilometer to 40 meters. The innermost domain reproduced tornado wind field shows a good agreement to the observed typical tornado and experimental results in average wind characteristics. In this study, not only the symmetric averaged wind characteristics tornado is compared with recent tornado wind field model; the spatial and temporal variation of tornado is also emphasized. Simulated multiple vortexes structures associated with central downdraft inside the tornado is observed. The importance of low level updraft to tilt horizontal vorticity to vertical vorticity is exhibited.
机译:F3超级龙卷风袭击了日本东部的筑波市,这是日本有史以来破坏性最强的龙卷风之一,造成了一场死亡和重大财产损失。为了探索现实条件下的龙卷风的风特征,已使用天气研究和预报模型(WRF)模型并成功地重新生成了该龙卷风过程。 WRF模型的仿真是通过三层嵌套域将水平网格分辨率从1公里降低到40米来进行的。在最里面的区域重现的龙卷风风场与观测到的典型龙卷风和平均风特征的实验结果显示出良好的一致性。在这项研究中,不仅将对称的平均风特征龙卷风与最近的龙卷风风场模型进行了比较;还强调了龙卷风的时空变化。观察到与龙卷风内部的中央向下气流相关的模拟的多个旋涡结构。表现出低水平上升气流使水平涡旋向垂直涡旋倾斜的重要性。

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