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作 者:龙训建[1] 翁薛柔 叶琰[1] 张逸轩[2] 徐廷兵[3] 叶勇[1] LONG Xunjian;WENG Xuerou;YE Yan;ZHANG Yixuan;XU Tingbing;YE Yong(College of Resources and Environment,Southwest University,Chongqing 400715,China;Chongqing Weather Modification Office,Chongqing 400074,China;Logistical Support Department,Southwest University,Chongqing 400715,China)
机构地区:[1]西南大学资源环境学院,重庆400715 [2]重庆市人工影响天气办公室,重庆400074 [3]西南大学后勤保障部,重庆400715
出 处:《水资源与水工程学报》2021年第6期19-26,共8页Journal of Water Resources and Water Engineering
基 金:中央高校基本科研业务费专项资金项目(XDJK2020C070);重庆市教育委员会科学技术研究项目(KJZD-K202100201)。
摘 要:基于重庆市32个国家气象站点的2009-2018年逐分钟降雨观测数据,开展侵蚀性降雨的雨量、历时、雨强及降雨侵蚀力特征值分析,探讨研究区侵蚀性降雨时空分布特征及雨情特点。结果表明:研究区多年平均侵蚀性降雨量、历时、雨强及发生次数分别占多年平均降雨量、历时、雨强及发生次数的75%、44%、55%和18%;侵蚀性降雨年内主要集中于5-9月,雨量、历时的年内分布呈双峰变化,雨强、发生次数和降雨侵蚀力年内变化则呈单峰特征;降雨侵蚀力年际变化幅度为-22%~27%。侵蚀性降雨各特征值在空间上表现出明显的区域差异性,主成分聚类分析方法将研究区划分为轻度、中度和重度3类降雨侵蚀区;研究区雨情基于K均值聚类分为3类,类Ⅰ为区域主要雨型,类Ⅲ为降雨侵蚀力最剧烈的雨型,类Ⅱ的雨量、雨强、历时以及降雨侵蚀力则介于类Ⅰ、类Ⅲ之间。Based on the minute-per-minute rainfall observation data of 32 national meteorological stations in Chongqing City from 2009 to 2018,the characteristics of amount,duration,intensity and erosivity of erosive rainfalls were analyzed to explore the spatiotemporal distribution characteristics and different patterns of erosive rainfalls in the study area.The results show that the amount,duration,intensity and occurrence frequency of the average annual erosive rainfall accounted for 75%,44%,55%and 18%of those of the average annual rainfall,respectively.Erosive rainfalls were mainly concentrated in May to September,of which the amount and duration showed a bimodal annual variation;whereas the intensity,occurrence frequency and rainfall erosivity presented a unimodal annual variation.The annual rainfall erosivity ranged from-22%to 27%,with a unimodal distribution.The various characteristic indices of erosive rainfalls showed obvious regional differences at different time scales.Then,principal component cluster analysis(PCA)was used to divide the study area into three types:light,moderate and severe rainfall erosion areas,and the rainfall patterns in the study area were divided into three categories based on K-means clustering,in which Category I was the dominant rainfall type in the region,CategoryⅢwas the rainfall type with the most severe erosivity,and the rainfall amount,intensity,duration and erosivity of Category II were between those of Category I and Category III.
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