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A Storm Modeling System as an Advanced Tool in Prediction of Well Organized Slowly Moving Convective Cloud System and Early Warning of Severe Weather Risk

机译:作为高级工具的风暴建模系统,用于预测组织良好的缓慢移动的对流云系统和恶劣天气风险的预警

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Short-range prediction of precipitation is a critical input to flood prediction and hence the accuracy of flood warnings. Since most of the intensive processes come from convective clouds-the primary aim is to forecast these small-scale atmospheric processes. One characteristic pattern of organized group of convective clouds consist of a line of deep convection resulted in the repeated passage of heavy-rain-producing convective cells over NW part of Macedonia along the line. This slowly moving convective system produced extreme local rainfall and hailfall in urban Skopje city. A 3-d cloud model is used to simulate the main storm characteristic (e.g., structure, intensity, evolution) and the main physical processes responsible for initiation of heavy rainfall and hailfall. The model showed a good performance in producing significantly more realistic and spatially accurate forecasts of convective rainfall event than is possible with current operational system. The output results give a good initial input for developing appropriate tools such as flooding indices and potential risk mapping for interpreting and presenting the predictions so that they enhance operational flood prediction capabilities and warnings of severe weather risk of weather services. Convective scale model-even for a single case used has proved significant benefits in several aspects (initiation of convection, storm structure and evolution and precipitation). The storm-scale model (grid spacing-1 km) is capable of producing significantly more realistic and spatially accurate forecasts of convective rainfall events than is possible with current operational systems based on model with grid spacing 15 km.
机译:降水的短程预报是洪水预报的关键输入,因此是洪水预警的准确性。由于大多数密集过程都来自对流云,因此主要目的是预测这些小规模的大气过程。有组织的对流云群的一个特征性模式是由一条深对流线组成,这导致产生大量雨水的对流细胞沿着该线在马其顿的西北部反复通过。这种缓慢移动的对流系统在斯科普里市区产生了极大的局部降雨和雹灾。使用3-d云模型来模拟主要的风暴特征(例如,结构,强度,演变)以及负责引发大雨和冰雹的主要物理过程。该模型在产生对流降雨事件的预报上要比当前操作系统更有效和空间精确,表现出良好的性能。输出结果为开发合适的工具(如洪水指数和潜在风险图,用于解释和呈现预测)提供了良好的初始投入,从而增强了洪水预测的操作能力,并警告了天气服务的恶劣天气风险。对流尺度模型-即使是单个案例,也已在多个方面(对流初始化,风暴结构以及演变和降水)证明了显着优势。与基于网格间隔为15 km的模型的当前操作系统相比,风暴尺度模型(网格间隔为1 km)能够产生对流降雨事件的更加真实和空间准确的预测。

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