高级检索
刘海文, 丁一汇. 华北汛期日降水特性的变化分析[J]. 大气科学, 2010, 34(1): 12-22. DOI: 10.3878/j.issn.1006-9895.2010.01.02
引用本文: 刘海文, 丁一汇. 华北汛期日降水特性的变化分析[J]. 大气科学, 2010, 34(1): 12-22. DOI: 10.3878/j.issn.1006-9895.2010.01.02
LIU Haiwen, DING Yihui. Analysis of Daily Precipitation Characteristics over North China during Rainy Seasons[J]. Chinese Journal of Atmospheric Sciences, 2010, 34(1): 12-22. DOI: 10.3878/j.issn.1006-9895.2010.01.02
Citation: LIU Haiwen, DING Yihui. Analysis of Daily Precipitation Characteristics over North China during Rainy Seasons[J]. Chinese Journal of Atmospheric Sciences, 2010, 34(1): 12-22. DOI: 10.3878/j.issn.1006-9895.2010.01.02

华北汛期日降水特性的变化分析

Analysis of Daily Precipitation Characteristics over North China during Rainy Seasons

  • 摘要: 基于中国740站逐日降水资料, 使用线性倾向估计、 Mann-Kendall突变检验等方法, 分析了华北汛期降水量、 5类汛期降水频率及其贡献率的趋势特征和年代际变化, 揭示出一些比较有意义的新事实, 结果如下: 华北汛期降水量、 5类降水频率及其贡献率都有一定的下降趋势, 华北汛期降水量下降趋势最明显。5类降水频率的下降趋势, 表现出明显的渐变特点, 其中, 小雨频率下降趋势最大, 暴雨频率和大暴雨频率的下降趋势并不显著。5类降水贡献率下降趋势中, 华北暴雨贡献率下降趋势最大。50年来, 华北汛期大雨贡献率最大, 接近于总降水的1/3。华北汛期降水量的多寡主要受其汛期大雨的频率和暴雨的贡献率影响。华北汛期降水量和暴雨贡献率都在1978年前后发生了年代际突变, 华北暴雨贡献率的年代际突变是造成华北汛期降水量发生年代际突变的内在因素。

     

    Abstract: Based on the daily precipitation data from 740 stations, by means of linear trend estimate, Mann-Kendall test method, the long-term trends and interdecadal variation of precipitation, frequency, contribution to the total rainfall over North China during rainy seasons are analyzed. Some new results are discovered as follows: the rainfall over North China during rainy seasons, and five kinds of precipitation frequency and contribution over North China during rainy seasons have a certain decreased trend with different decreased rates. The most obvious decreased trend is the rainfall over North China during rainy seasons. The long-term decreased trend of the five kinds of precipitation frequency has obvious characteristic of gradual change, and the decreased trend of light rain frequency is biggest while the decreased trend of torrential rain and excessively heavy rainfall frequency is not significant. Meanwhile, the decreased trend of contribution of heavy rain to the total rainfall over North China are biggest. The biggest contribution to the total rainfall over North China is from heavy rain and close to one-third of the total rainfall in the past 50 years. The rainfall over North China during rainy seasons is mainly influenced by the heavy rain frequency and the excessively heavy rainfall contribution. The interdecadal abrupt change took placed in 1978 for both rainfall and excessively heavy rainfall contribution over North China during the rainy season, so the interdecadal abrupt change of excessively heavy rainfall contribution during rainy seasons results in the interdecadal abrupt change of rainfall over North China.

     

/

返回文章
返回