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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Circulation weather types and cloud-to-ground flash density over the Iberian Peninsula
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Circulation weather types and cloud-to-ground flash density over the Iberian Peninsula

机译:伊比利亚半岛上的环流天气类型和云对地闪光密度

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摘要

Based on the use of an objective classification method for the general atmospheric circulation observed over the Iberian Peninsula for the 1990-98 period, we have characterized the daily circulation by means of a set of indices associated with the direction and vorticity of the geostrophic flow. We analyse the synoptic characteristics of the types of circulation obtained, gaining statistical information about the most frequent basic situations for the annual and seasonal periods. We show how the anticyclone situation (A) predominates in winter, spring and autumn, whereas in summer the most frequent weather corresponds to pure easterly weather (E) followed by cyclonic weather (C). We report the findings of a comparative study between the frequencies of the daily values of the dominant types of circulation and the corresponding daily values of the number of cloud-to-ground flashes over the Iberian Peninsula between 1992 and 1994. Each synoptic situation is described by a set of characteristics that explains the development of the convective processes. A high degree of correspondence was obtained, especially for the months between May and October, in which major storm activity occurs (Pearson correlation coefficient: 0.76). All the results show that convective processes, which generate storm activity, can be appropriately explained in terms of the variability of a small number of general synoptic situations.
机译:基于客观分类方法对1990-98年伊比利亚半岛整个大气环流的观测,我们通过与地转流的方向和涡度相关的一组指标来描述了日常环流。我们分析了所获得的环流类型的天气特征,获得了有关年度和季节性最常见基本情况的统计信息。我们显示了冬季,春季和秋季,反气旋情况(A)如何占主导地位,而夏季,最频繁的天气对应于纯东风(E),然后是气旋天气(C)。我们报告了在1992年至1994年之间,伊比利亚半岛上主要的循环类型的每日值的频率与相应的每日地面到地面云闪次数的比较之间的比较研究结果。通过解释对流过程发展的一系列特征。高度对应,特别是在5月至10月之间发生大风暴活动的月份中(Pearson相关系数:0.76)。所有结果表明,产生风暴活动的对流过程可以根据少量一般天气情况的变化来适当地解释。

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