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Numerical Experiments of Meso-α-Scale Precipitation Systems under Baiu-Front-Like Idealized Environments

机译:Baiu-Front-like理想环境下中尺度α降水系统的数值实验

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References(18) To investigate the variability of the structure and evolution of meso-α-scale precipitation systems generated in the Baiu frontal zone, numerical experiments using a cloud-resolving non-hydrostatic model were performed with idealized Baiu-front-like environments. The environment was constructed based on hydrostatic and geostrophic balances, and temperature and relative humidity were designed by using Gaussian functions to realize the frontal structure and moist conveyor belt in the lower atmosphere. In order to generate meso-α-scale precipitation systems, temperature perturbation associated with a shallow depression was introduced. Long-lived band-shaped meso-α-scale precipitation systems with the internal multiscale structures as are often observed in the Baiu frontal zone were simulated under the given simplified environments. The variability of features of the meso-α-scale precipitation systems with respect to relative humidity in the middle troposphere in the Baiu frontal zone was examined as an example. The moister environment produced the more rainfall. Additionally, rainfall was intensified under a specific humidity condition.
机译:参考文献(18)为了研究在Baiu锋区产生的中α尺度降水系统的结构和演化的可变性,在理想化的Baiu-front-like环境下使用云解析非静水模型进行了数值实验。根据静水压力和地转平衡来构建环境,并利用高斯函数设计温度和相对湿度,以在较低的大气层中实现正面结构和潮湿的输送带。为了产生中α尺度的降水系统,引入了与浅洼区有关的温度扰动。在给定的简化环境下,模拟了在Baiu额叶带经常观察到的具有内部多尺度结构的长寿命带状中观α尺度降水系统。以Baiu额叶中部对流层中尺度相对湿度为例,研究了中尺度α降水系统的特征变化。潮湿的环境产生了更多的降雨。另外,在特定的湿度条件下降雨增加。

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