双月刊

ISSN 1006-9895

CN 11-1768/O4

陕西汛期5类天气环流降水雨滴谱分布统计特征对比研究
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作者单位:

1.中山大学大气科学学院;2.中国科学院地理科学与资源研究所陆地水循环及地表过程重点实验室;3.陕西省气象台

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陕西省自然科学基础研究计划项目(2023JCQN0341),国家重点研发计划项目(2022YFC3002904,2022YFC3004101),海南省重点研发计划项目(ZDYF2023SHFZ125)


Comparative Study on the Statistical Characteristics of Raindrop Spectral Distribution of Five Types of Weather Circulation Precipitation in Shaanxi Flood Season
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Affiliation:

1.School of Atmospheric Sciences, Sun Yat-Sen University;2.Key Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences

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    摘要:

    雨滴谱作为直接描述雨滴尺寸、数量等特征的高频次观测资料,已被广泛应用到不同天气、不同类型雨滴变化的精细化评估分析中。本研究利用2019-2022年陕西地区近4年雨滴谱观测资料,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>5mm h-1的降水对过程总雨量贡献度在各环流之间差异明显,雨滴在不同直径区间的数浓度及降雨率贡献程度不同是带来这种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。不同环流暴雨降水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>5mm 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Dm-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Z-R经验关系的基础上,基于雨滴谱优化拟合了陕西各环流降水的Z-R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, as a high-frequency observation data that directly describes the characteristics of raindrop size and quantity, has been widely used in the fine evaluation and analysis of raindrop changes in different weather conditions and types. The study utilized raindrop spectrum observation data from 2019 to 2022 in the Shaanxi Province. We have analyzed the overall characteristics of precipitation under the influence of five weather circulations, the drop spectra characteristics of rainstorm and non-rainstorm processes, and the drop spectra characteristics of convective precipitation and stratiform precipitation. The results indicate that the contribution of precipitation with rainfall rate>5mm h-1 to the total rainfall of the process varies significantly among different circulation systems. The main reason for this situation is the difference in the number concentration and contribution of raindrops in each diameter intervals. For example, the southwest airflow type is often characterized by stable precipitation formed by long-term high concentration small raindrops, while the northwest airflow type is characterized by strong precipitation formed by short-term high concentration large raindrops. The characteristics difference of drop spectrum between different circulation rainstorm and non-rainstorm further increase, and heavy rainfall have a significant promoting effect on raindrop spectral parameters. From the variation of number concentration with diameter, the number proportion and diameter spectral width of convective precipitation raindrops with rainfall rate>5mm h-1 in the rainstorm are generally higher than those of non-rainstorm. The distribution range and magnitude of Dm-Nw 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 of convective precipitation in Shaanxi tends to have oceanic convective precipitation characteristics. A few continental convective precipitation occur in flat straight airflow weather or northwest airflow weather. Based on the above analysis, this study differs from the traditional Z-R empirical relationship and optimizes the fitting of Z-R precipitation estimation equations for various circulation precipitation based on raindrop spectra, which helps to improve the accuracy of radar precipitation estimation in different weather scenarios in the local area in Shaanxi.

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  • 收稿日期:2023-09-05
  • 最后修改日期:2024-03-12
  • 录用日期:2024-04-03
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