干旱气象 ›› 2019, Vol. 37 ›› Issue (6): 892-898.

• 论文 • 上一篇    下一篇

济南地区小时强降水变化特征

董旭光1,邱粲2,1,刘焕彬1,陈艳春1,叶殿秀3,李胜利4   

  1. 1.山东省气候中心,山东济南250031;2.上海师范大学地理系,上海200234;
    3.国家气候中心,北京100081;4.山东省济南市气象局,山东济南250102
  • 出版日期:2019-12-31 发布日期:2020-01-02
  • 通讯作者: 刘焕彬(1964— ),男,高级工程师,主要从事气候应用研究工作. E-mail:hb_liu@163.com。
  • 作者简介:董旭光(1979— ),男,硕士,高级工程师,主要从事气候变化和气候应用研究工作. E-mail:dongxugg@sina.com。

Characteristics of Hourly Heavy Precipitation Changes in Jinan Area

DONG Xuguang1, QIU Can2,1, LIU Huanbin1, CHEN Yanchun1, YE Dianxiu3, LI Shengli4#br#   

  1. 1. Shandong Climate Center, Jinan 250031, China; 2. Department of Geography, Shanghai Normal
     University, Shanghai 200234, China; 3. National Climate Center, Beijing 100081, China;
    4. Jinan Meteorological Bureau of Shandong Province, Jinan 250102, China
  • Online:2019-12-31 Published:2020-01-02

摘要: 利用济南地区2008—2017年3—11月50个区域自动站逐时降水数据,研究该区域雨强超过10.0、20.0、30.0 mm·h-1的降水量时空变化特征。结果表明:济南全区小时强降水受城市化、地形和盛行风的影响显著,济南城区、南部山区、长清山前地带、商河等地降水偏多,济南市区下风向近郊、章丘、济阳、平阴一带强降水偏少。7、8月济南地区小时强降水最多,雨强≥20.0 mm·h-1的月平均降水量均超过40.0 mm,贡献率均超过25.0%。小时强降水日变化呈双峰双谷特征,11:00和23:00前后为强降水最少时段,04:00—05:00和14:00—21:00是强降水较多时段。大部分站点强降水峰值出现在午夜至凌晨和下午至傍晚时段。

关键词: 小时强降水, 时空变化, 日变化, 济南地区

Abstract: Based on the hourly precipitation data of 50 automatic meteorological stations in Jinan area from March to November during 2008-2017, the temporal and spatial variation characteristics of precipitation with rainfall intensity over 10.0, 20.0, 30.0 mm·h-1 were studied. The results show that the hourly heavy precipitation in Jinan was affected by urbanization, topography and prevailing winds. There were more precipitation in Jinan urban area, southern mountainous area, Shanghe county and piedmont region in Changqing district, while there were relatively less precipitation in the downwind area of the suburbs, Zhangqiu district, Jiyang district and Pingyin county. Hourly heavy precipitation occurred most in July and August, monthly average precipitation with rain intensity equal to or more than 20.0 mm·h-1 was over 40.0 mm and its contribution rate was over 25.0%. The diurnal variation of heavy precipitation was characterized by double peaks and double valleys. The minimum precipitation period was around 11:00 and 23:00, and the maximum precipitation period was 04:00-05:00 and 14:00-21:00. Most sites had peak precipitation from midnight to early morning and from afternoon to evening.

Key words: heavy precipitation, spatial and temporal changes, diurnal variation, Jinan area

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