干旱气象 ›› 2019, Vol. 37 ›› Issue (3): 370-.

• 论文 • 上一篇    下一篇

渡河流域面雨量时空分布特征及雨季转换指标

郭洁1,2,宋雯雯1,2,郑昊1,2,刘新超1,2   

  1. 1.四川省高原与盆地暴雨旱涝灾害四川省重点实验室,四川成都610072;
    2.四川省气象服务中心,四川成都610072
  • 出版日期:2019-06-28 发布日期:2019-07-01
  • 作者简介:郭洁(1981— ),女,四川峨眉人,高级工程师,主要从事专业气象服务和研究.E-mail:guojie126@163.com。
  • 基金资助:
    高原与盆地暴雨旱涝灾害四川省重点实验室2018年度科技发展基金项目(2018-重点-03,2018-青年-10)资助

Analysis on Spatial and Temporal Distribution of Areal Precipitation in Dadu River Basin and Rainy Season Transition Indexes

GUO Jie1,2, SONG Wenwen1,2, ZHENG Hao1,2, LIU Xinchao1,2   

  1. 1. Heavy Rain and Drought-Flood Disasters in Plateau and Basin Key Laboratory of Sichuan Province,
     Chengdu 610072, China; 2. Sichuan Meteorological Service Centre, Chengdu 610072, China
  • Online:2019-06-28 Published:2019-07-01

摘要: 利用1961—2016年大渡河流域15个气象站逐日降水资料,采用算术平均法计算上、中、下游三个分段流域的面雨量,对其时空分布特征进行分析,计算流域内雨季开始及结束期。结果表明:(1)大渡河中、上游面雨量呈上升趋势,下游呈下降趋势,下游年降水量相对变率和极差最大,其次是中游,上游最小;夏季流域面雨量最大,占全年降水的50%~60%。5—9月流域面雨量在100~200 mm之间,11月至翌年2月在5~20 mm之间,流域内面雨量峰值出现时间由北向南延迟,上、中、下游相差近1个月。(2)依据雨季转换指标计算出的雨季开始及结束期比依据强降水计算的更稳定,大渡河流域下游进入雨季最早,其次是中游,上游最晚,而上游雨季结束最早,其次是中游,下游最晚,上、中、下游雨季持续时间分别为172 d、182 d和195 d。(3)当上游出现强降水时,中、下游很少同时出现强降水,当下游出现强降水时,中游经常同时也出现强降水。

关键词: 大渡河流域, 面雨量, 雨季转换, 强降水

Abstract: Based on the daily precipitation data of 15 meteorological stations in the Dadu River Basin during 1961-2016, the areal precipitation of the upper, middle and lower reaches of the Dadu River Basin was caculated by using arithmetic average method. And the spatial and temporal distribution characteristics of its areal precipitation were analyzed. In addition, the beginning and ending date of the rainy season in the Dadu River Basin were calculated in this article. The results are as follows: (1) The areal precipitation of the middle and upper reaches of the Dadu River Basin showed an upward trend, while that of the lower reaches showed a downward trend. The relative variability and range of annual precipitation in the lower reaches were the largest, followed by the middle and the upper reaches. The areal rainfall was maximum in the Dadu River Basin in summer, it was about 50%-60% of the annual precipitation. The monthly average areal rainfall in the Dadu River Basin was 100-200 mm from May to September, and 5-20 mm from November to the following February. The peak of areal rainfall in the Dadu River Basin from north to south was delayed about a month. (2) The beginning and ending period of the rainy season calculated by the conversion index of the rainy season was more stable than that calculated by the heavy rainfall. The lower reaches of the Dadu River Basin entered the rainy season at the earliest, followed by the middle and the upper reaches. The upper reaches of the Dadu River Basin ended the rainy season at the earliest, followed by the middle and the lower reaches. The duration of rainy season in the upper, middle and lower reaches were 172 days, 182 days and 195 days, respectively. (3) Under the condition of heavy precipitation occurring in the upper reaches of the Dadu River Basin, the probability of heavy precipitation occurring in the middle and lower reaches at the same time was very small. Nevertheless, the heavy precipitation often occurred in the middle reaches of the Dadu River Basin at the same time when heavy precipitation occurred in the lower reaches.

Key words: Dadu River Basin, areal precipitation, rainy season transition, heavy precipitation

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