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陕西省汛期5类天气环流降水雨滴谱分布统计特征对比

Comparative on the Statistical Characteristics of Raindrop Spectral Distribution in Five Types of Weather Circulation Precipitation during the Flood Season in Shaanxi Province

  • 摘要: 雨滴谱作为可以直接描述雨滴尺寸、数量等特征的高频次观测资料,广泛应用到对不同天气、不同类型雨滴变化的精细化评估分析中。本研究利用2019~2022年陕西地区雨滴谱资料,分析了5种天气环流影响下陕西降水总体特征、暴雨过程和非暴雨过程滴谱特征以及对流降水和层云降水滴谱特征。研究结果表明,雨强>5 mm h−1的降水对过程总雨量贡献度在各环流之间差异明显,不同直径区间雨滴数浓度及降雨率的贡献程度不同是形成总体特征差异的主要原因,例如,西南气流型多为长时间高浓度小雨滴形成稳定降水,西北气流型多为短时间高浓度大雨滴形成强降水。不同环流暴雨与非暴雨降水之间的滴谱差异特征进一步增大,高雨强降水对雨滴谱参量有明显促进作用。雨滴数浓度随直径变化的特征显示,各环流天气暴雨过程中雨强>5 mm h−1的对流降水雨滴数量比例和直径谱宽普遍高于非暴雨降水。各环流类型的对流降水之间和层云降水之间的质量加权平均直径(Dm)—标准化截距参数(Nw)分布范围、量级等特征接近,差别在于平均值点及大值区位置。对比昭苏、珠海及帕劳岛等类似地区对流降水特征,陕西大部分对流降水偏向海洋性对流降水特征,少数大陆性对流降水多出现在平直气流型和西北气流型天气中。本研究基于上述分析,在传统雷达反射率因子(Z降水率(R)经验关系的基础上,通过雨滴谱参数优化拟合了陕西各环流降水的ZR估测降水关系式,有助于提升当地不同天气场景下雷达估测降水的准确率。

     

    Abstract: The raindrop spectrum, a high-frequency observational dataset that directly describes raindrop size and quantity, has been widely used for precise evaluation and analysis of raindrop variations across different weather conditions and types. The study utilized raindrop spectrum observation data from 2019 to 2022 in Shaanxi Province. The authors analyzed the overall precipitation characteristics under the influence of five weather circulations, the drop spectra characteristics of rainstorm and non-rainstorm processes, and those of convective precipitation and stratiform precipitation. The results indicate that the contribution of precipitation with a rainfall rate>5 mm h−1 to total process rainfall varies considerably across different circulation systems. This variation primarily stems from differences in the number concentration and contribution of raindrops within each diameter interval. For example, the southwest airflow type is often characterized by stable precipitation, formed by long-term, high-concentration small raindrops, whereas the northwest airflow type tends to produce intense precipitation, driven by short-term, high-concentration large raindrops. The differences in drop spectrum characteristics between rainstorm and non-rainstorm circulations become more pronounced, with heavy rainfall significantly enhancing raindrop spectral parameters. The variation of number concentration with diameter indicates that the proportion and spectral width of convective precipitation raindrops with a rainfall rate>5 mm h−1 are generally higher in rainstorms than in non-rainstorms. The distribution range and magnitude of DmNw between convective precipitation and stratiform precipitation are nearly similar, with differences in the location of mean and high-value areas. Compared with similar regions such as Zhaosu, Zhuhai, and Palau Island, most convective precipitation in Shaanxi exhibits oceanic convective precipitation characteristics. A few instances of continental convective precipitation occur in flat, straight airflow weather or northwest airflow weather. Based on this analysis, the study diverges from the traditional Z–R empirical relationship and optimizes the fitting of Z–R precipitation estimation equations for various circulation precipitation types using raindrop spectra. This optimization enhances the accuracy of radar precipitation estimation across different weather scenarios in Shaanxi.

     

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