罗希昌, 杨彬, 张玉生, 王传辉, 姚叶青. 安徽省分钟降雨率分布特征[J]. 电波科学学报, 2020, 35(6): 908-913. doi: 10.13443/j.cjors.2020103001
      引用本文: 罗希昌, 杨彬, 张玉生, 王传辉, 姚叶青. 安徽省分钟降雨率分布特征[J]. 电波科学学报, 2020, 35(6): 908-913. doi: 10.13443/j.cjors.2020103001
      LUO Xichang, YANG Bin, ZHANG Yusheng, WANG Chuanhui, YAO Yeqing. Distribution characteristics of minute rainfall rate in Anhui Province[J]. CHINESE JOURNAL OF RADIO SCIENCE, 2020, 35(6): 908-913. doi: 10.13443/j.cjors.2020103001
      Citation: LUO Xichang, YANG Bin, ZHANG Yusheng, WANG Chuanhui, YAO Yeqing. Distribution characteristics of minute rainfall rate in Anhui Province[J]. CHINESE JOURNAL OF RADIO SCIENCE, 2020, 35(6): 908-913. doi: 10.13443/j.cjors.2020103001

      安徽省分钟降雨率分布特征

      Distribution characteristics of minute rainfall rate in Anhui Province

      • 摘要: 利用安徽省2017—2019年81个国家级气象站实测分钟降雨率资料,统计站点分钟降雨率累积分布,对安徽省分钟降雨率的时空分布特征进行分析,并将实测降雨率与ITU降雨率模型预测结果进行对比.结果表明:安徽省山区的分钟降雨率累积分布整体上高于其他地区,淮北平原东部在小于0.03%时间概率点时呈现出较高分钟降雨率累积分布;山区受地形降雨影响,高海拔处分钟降雨率总体上高于低海拔处;平原地区的R(0.01)年际变化较其他地区显著;2017年、2018年和2019年的降雨最坏月份分别为8月、7月和6月.实测分钟降雨率分布与ITU模型预测结果总体上保持一致,在0.03%时间概率点以内,模型预测结果整体偏低;在淮北平原和山区高海拔处,模型预测结果误差较大.

         

        Abstract: Using the measured minute rainfall data of 81 national meteorological stations in Anhui Province from 2017 to 2019, we calculate the cumulative distribution of minute rainfall rate at the station, and analyze the temporal and spatial distribution characteristics of minute rainfall rate in Anhui Province. Finally, the measured rainfall rate is compared with the prediction result of the ITU rainfall rate model. The results show that the cumulative distribution of minute rainfall rate in mountainous areas in Anhui Province is generally higher than that in other regions. The eastern part of the Huaibei Plain shows a higher cumulative distribution of minute rainfall rates within 0.03% of the time percentage. In mountainous areas, affected by terrain rainfall, the minute rainfall rate at high altitudes is generally higher than that at low altitudes. The interannual variability of R(0.01) in the plain area is more significant than that in other areas. The worst months of the province's rainfall rate are August, July and June. The distribution of the measured minute rainfall rate is generally consistent with the ITU model prediction results. Within 0.03% of the time, the model prediction results are generally low; in the Huaibei Plain and high altitude areas in the mountains, and the model prediction results have large errors.

         

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