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首页> 外文期刊>Annales Geophysicae >A numerical study of cell merger over Cuba - Part Ⅰ: implementation of the ARPS/MM5 models
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A numerical study of cell merger over Cuba - Part Ⅰ: implementation of the ARPS/MM5 models

机译:古巴细胞合并的数值研究-第一部分:ARPS / MM5模型的实现

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On 21 July 2001 a number of severe storms developed over the region of Camaguey, Cuba, which were observed by radar. A numerical simulation was performed in order to realistically reproduce the development of the storms observed that day. The mesoscale model MM5 was used to determine the initial, boundary and update conditions for the storm-scale simulation with the model ARPS. Changes to the source code of ARPS were made in order to assimilate the output from the MM5 as input data and a new land-use file with a 1-km horizontal resolution for the Cuban territory was created. A case representing the merger between cells at different stages of development was correctly reproduced by the simulation and is in good agreement with radar observations. The state of development of each cell, the time when the merger occurred, starting from the formation of clouds, the propagation motion of the cells and the increase in precipitation, due to the growth of the area after the merger, were correctly reproduced. Simulated clouds matched the main characteristics of the observed radar echoes, though in some cases, reflectivity tops and horizontal areas were overestimated. Maximum reflectivity values and the heights where these maximum values were located were in good agreement with radar data, particularly when the model reflectivity was calculated without including the snow. The MM5/ARPS configuration introduced in this study, improved sensibly the ability to simulate convective systems, thereby enhancing the local forecasting of convection in the region.
机译:2001年7月21日,在古巴的卡马圭地区爆发了几场严重的风暴,并用雷达对其进行了观测。为了真实再现当天观察到的风暴的发展,进行了数值模拟。中尺度模型MM5用于确定使用ARPS模型进行的风暴尺度模拟的初始条件,边界条件和更新条件。更改了ARPS的源代码,以将MM5的输出用作输入数据,并为古巴领土创建了一个水平分辨率为1 km的新土地使用文件。通过仿真可以正确再现一个代表处于不同发展阶段的单元之间合并的案例,并且该案例与雷达观测非常吻合。正确地复制了由于合并后面积的增长而从云的形成开始的每个单元的发展状态,合并发生的时间,单元的传播运动以及降水的增加。模拟的云与观测到的雷达回波的主要特征相符,尽管在某些情况下,反射率的顶部和水平区域被高估了。最大反射率值和这些最大值所在的高度与雷达数据高度吻合,尤其是在计算模型反射率而未包括雪的情况下。这项研究中引入的MM5 / ARPS配置显着提高了模拟对流系统的能力,从而增强了该地区对流的局部预报。

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