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Spatial and temporal distribution of hailstorms in the Alpine region: a long-term, high resolution, radar-based analysis

机译:高山地区冰雹的时空分布:长期,高分辨率,基于雷达的分析

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This article presents a 13-year hail climatology for Switzerland based on volumetric radar reflectivity. Two radar-based hail detection products that are used operationally at MeteoSwiss, namely the Probability of Hail (POH) and the Maximum Expected Severe Hail Size (MESHS), have been reprocessed for the extended convective season (April-September) between 2002 and 2014. The result of these two products is a comprehensive hail distribution map, which highlights regional and local-scale hail characteristics. The map of the annual number of hail days shows a high spatial variability and several maxima over the foothills north and south of the Alps as wells as over the Jura mountains. Directly over the Alps hail frequency exhibits a minimum. Annual hail anomalies show a pronounced variability, which suggests that hail occurrence is strongly controlled by large-scale weather patterns. Furthermore, hail probability exhibits a strong seasonal and diurnal cycle with a maximum in July in the late afternoon. The hail peak over the northern pre-alpine region occurs approximately two hours earlier compared to the south. A possible explanation is the trigger mechanism between the cold pool initiated by early convective cells over the Jura mountains and the development of cells on the northern slope of the Alps. Since radar-based hail signals are only indirect measurements, statistical verification of the hail detection algorithms is crucial. Damage reports from an automobile insurance company are used as an independent dataset. Verification results confirm that radar-based hail algorithms provide valuable information on hail probability. Finally, the synoptic-scale hail-driving weather conditions are investigated using a weather type classification based on upper-air flow direction and mean pressure from a numerical weather prediction model. The results show that six out of nine main synoptic-scale patterns favour the development of hailstorms in Switzerland.
机译:本文介绍了基于体积雷达反射率的瑞士13年冰雹气候。在MeteoSwiss上使用的两种基于雷达的冰雹检测产品,即冰雹概率(POH)和最大预期严重冰雹尺寸(MESHS),已经过重新处理,以用于2002年至2014年之间的延长对流季节这两个产品的结果是一个完整的冰雹分布图,突出显示了区域和地方范围的冰雹特征。每年的冰雹天数地图显示出高度的空间变异性,并且在阿尔卑斯山以南和北部的丘陵以及侏罗山上都达到了几个最大值。直接在阿尔卑斯山上出现的冰雹频率最低。每年的冰雹异常表现出明显的可变性,这表明冰雹的发生受到大规模天气模式的强烈控制。此外,冰雹概率表现出强烈的季节性和昼夜周期,7月下旬达到最大值。与南部相比,北部高山前地区的冰雹峰出现的时间要早​​两个小时。一个可能的解释是侏罗山上的早期对流细胞引发的冷池与阿尔卑斯山北坡上的细胞发育之间的触发机制。由于基于雷达的冰雹信号只是间接测量,因此冰雹检测算法的统计验证至关重要。汽车保险公司的损坏报告用作独立数据集。验证结果证实,基于雷达的冰雹算法可提供有关冰雹概率的有价值的信息。最后,使用天气类型分类,基于高层气流方向和来自数值天气预报模型的平均压力,研究了天气尺度下的冰雹驾驶天气状况。结果表明,在9个主要天气尺度模式中,有6个有利于瑞士冰雹的发展。

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