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Spatio-temporal distribution of the rainstorm in the east side of the Helan Mountain and the possible causes of its variability

机译:Helan山东东侧暴雨的时空分布及其变异性的可能原因

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摘要

Compared with other arid areas, the convective rainstorm occurs more easily in the east side of the Helan Mountain, which is characterized by the short duration, large intensity, high precipitation efficiency and significant local distribution. In this paper, the 5-min and hourly precipitation at 512 regional automatic weather stations and other high-resolution observation data are used to analyze the spatio-temporal distribution and evolution characteristics of the rainstorm in the east side of the Helan Mountain during 2006 and 2019. Then, based on the daily precipitation data at 12 national observation stations, the rainstorm characteristics in this region during 1951 and 2005 are analyzed. On this basis, the rainstorm characteristics in the two periods are compared and studied. Finally, the possible causes of the distribution characteristics of rainstorm are initially discussed. The results show that the rainstorm with large magnitude and high intensity is mainly located in the mountainous region, and it mainly occurs in July with a high frequency period from afternoon to the first half of the night. Compared with 1951-2005, in 2006-2019 the rainstorm frequency, intensity and extremity are all increased, and the nocturnal and topographic features are more significant. The spatio-temporal distribution of rainstorm in the east side of the Helan Mountain is closely related to the nighttime enhancement of the low-level southeasterly jet and the interaction between the low-level jet and the mountainous topography. In the windward slope of the Helan Mountain, the interaction between the low-level jet and the mountainous topography could trigger or enhance the mesoand small-scale rainstorm systems, which would favor the occurrence of rainstorm. Overall, the conclusions in this study can deep the understanding of the rainstorms in the Helan Mountain, which could provide a reference for the monitoring and warning of rainstorms in this region.
机译:与其他干旱地区相比,对流暴雨在贺兰山的东侧更容易发生,其特征在于持续时间短,强度大,降水效率高,局部分布。在本文中,512个区域自动气象站和其他高分辨率观察数据的5分钟和每小时降水用于分析2006年贺兰山东侧的时空分布和进化特征2019年。然后,根据12个国家观察站的日降水数据,分析了1951年和2005年该地区的暴雨特性。在此基础上,比较和研究了两个时期的暴雨特性。最后,最初讨论了暴雨分布特征的可能原因。结果表明,大幅度和高强度的暴雨主要位于山区,主要发生在7月份,从下半年到上半年的频率高。与1951-2005相比,2006 - 2019年暴雨频率,强度和肢体都有增加,夜行和地形特征更为显着。贺兰山东侧的暴雨的时空分布与低级东南喷射的夜间增强以及低级喷射与山区地形之间的互动密切相关。在Helan Mountain的迎风斜率中,低级喷射和山地地形之间的相互作用可以触发或增强中间和小型暴雨系统,这将有利于暴雨的发生。总体而言,本研究的结论可以深入了解贺兰山的暴雨,这可以为该地区的暴雨监测和警告提供参考。

著录项

  • 来源
    《Atmospheric research》 |2021年第4期|105469.1-105469.16|共16页
  • 作者单位

    CMA Key Lab Meteorol Disaster Monitoring & Early Warn Yinchuan 750002 Ningxia Peoples R China|Ningxia Key Lab Meteorol Disaster Prevent & Mitig Yinchuan 750002 Ningxia Peoples R China|Ningxia Meteorol Observ Yinchuan 750002 Ningxia Peoples R China;

    CMA Key Lab Meteorol Disaster Monitoring & Early Warn Yinchuan 750002 Ningxia Peoples R China|Ningxia Key Lab Meteorol Disaster Prevent & Mitig Yinchuan 750002 Ningxia Peoples R China|Ocean Univ China Inst Adv Ocean Studies Key Lab Phys Oceanog Qingdao Natl Lab Marine Sci & Technol Qingdao 266100 Peoples R China;

    CMA Key Lab Meteorol Disaster Monitoring & Early Warn Yinchuan 750002 Ningxia Peoples R China|Ningxia Key Lab Meteorol Disaster Prevent & Mitig Yinchuan 750002 Ningxia Peoples R China;

    CMA Key Lab Meteorol Disaster Monitoring & Early Warn Yinchuan 750002 Ningxia Peoples R China|Ningxia Key Lab Meteorol Disaster Prevent & Mitig Yinchuan 750002 Ningxia Peoples R China|Ningxia Meteorol Observ Yinchuan 750002 Ningxia Peoples R China;

    CMA Key Lab Meteorol Disaster Monitoring & Early Warn Yinchuan 750002 Ningxia Peoples R China|Ningxia Key Lab Meteorol Disaster Prevent & Mitig Yinchuan 750002 Ningxia Peoples R China|Ningxia Meteorol Observ Yinchuan 750002 Ningxia Peoples R China;

    CMA Key Lab Meteorol Disaster Monitoring & Early Warn Yinchuan 750002 Ningxia Peoples R China|Ningxia Key Lab Meteorol Disaster Prevent & Mitig Yinchuan 750002 Ningxia Peoples R China|Ningxia Meteorol Observ Yinchuan 750002 Ningxia Peoples R China;

    CMA Key Lab Meteorol Disaster Monitoring & Early Warn Yinchuan 750002 Ningxia Peoples R China|Ningxia Key Lab Meteorol Disaster Prevent & Mitig Yinchuan 750002 Ningxia Peoples R China|Ningxia Meteorol Observ Yinchuan 750002 Ningxia Peoples R China;

    CMA Key Lab Meteorol Disaster Monitoring & Early Warn Yinchuan 750002 Ningxia Peoples R China|Ningxia Key Lab Meteorol Disaster Prevent & Mitig Yinchuan 750002 Ningxia Peoples R China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Rainstorm; Spatio-temporal distribution; Topographic influence; Low-level jet; East side of the Helan Mountain;

    机译:暴雨;时空分布;地形影响;低级喷射;贺兰山的东侧;

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