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ERA5-Land强降水极值位置不确定性的统计分析

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利用中国 1981-2019年 5-9月 665个台站的观测资料以及全球降水观测计划(Global Precipitation Meas-urement,GPM)反演的降水格点资料,针对东部地区 97个台站 224个强降水事件(日降水量超过 250 mm),统计了 0.1°空间分辨率的ERA5-Land再分析资料中降水极值位置和降水量的偏差.结果表明:① 在以台站为中心的9×9网格的矩形区域内存在强降水极值中心的个例有 123个(占总个例数的 54.9%),其落点位于站点所在网格及相邻网格的有 45个(占比 36.6%),偏离的距离在 4个网格之内的则达到 119个(占比 96.7%),即落点偏差绝大多数在 40 km内.从方位上看,主要的偏离方位是偏北(占比 30.1%),这证明了模拟强降水极值中心的落点偏差大多数没有超出中尺度的范围,且普遍偏北;② GPM反演降水中约 35%个例的站点位于强降水极值中心所在网格或相邻网格内,存在极值中心的 68场强降水对应的ERA5-Land极值中心偏差主要集中在 4个网格范围内(占比94.1%),且主要偏北(占比 31.7%);③ 如果考虑强降水极值中心位置的偏差对降水进行订正,则能够减少ERA5-Land降水量偏差 37.7 mm(12.6%),这证明了考虑强降水位置偏差,能够在考虑模拟强降水强度偏弱的同时,进一步减少预报误差.强降水极值位置的不确定性,对于极端降水事件的风险及预警范围有参考意义.
Statistical analysis of uncertainty in the location of ERA5-Land heavy precipitation extremes
Using the observation data from 665 stations in May-September 1981-2019 in China and the precip-itation grid data from the Global Precipitation Measurement(GPM)inversion,for 224 heavy precipitation events(daily precipitation exceeding 250 mm)at 97 stations in the eastern region,the deviation in the location of precipita-tion extremes and the precipitation amount in the ERA5-Land reanalysis data with 0.1 degree spatial resolution were counted.The results show that:1)There are 123 cases(54.9%of the total cases)of heavy precipitation extreme centers in the rectangular area of 9×9 grid centered on the station,45 cases(36.6%)of which have their fallout points located in the grid where the station is located and the adjacent grids,and 119 cases(96.7%)of which have their deviation within 4 grids,and the majority of the predicted precipitation extreme centers are within 40 km.In terms of orientation,the predominant deviation is toward the north(30.1%),indicating that most of the fallout deviation of the simulated extreme precipitation centers do not beyond the mesoscale range and tend to be northward;2)Approximately 35%of the stations in the GPM inversion precipitation are located in the grid where the extreme center of heavy precipitation is located or in the adjacent grid,and the deviation from the ERA5-Land extreme center corresponding to the 68 heavy precipitation events with the existence of extreme centers are mainly concentrated within 4 grids(94.1%of the total)and mainly to the north(31.7%of the total);3)If the precipitation is revised by considering the deviation of the location of the extreme center of heavy precipitation,it is able to reduce the ERA5-Land precipitation deviation by 37.7 mm(12.6%),which proves that considering the deviation of the location of heavy precipitation can further reduce the forecast error while taking into account the underestimation of simulated precipitation intensity.The uncertainty in the loca-tion of the heavy precipitation extremes is informative for the risk and warning areas of extreme precipitation events.

heavy precipitationposition deviationERA5-LandChina

王子晴、董雪晨、龚道溢

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北京师范大学地表过程与资源生态国家重点实验室,北京 100875

北京师范大学环境演变与自然灾害教育部重点实验室,北京 100875

应急管理部-教育部减灾与应急管理研究院,北京 100875

北京师范大学地理科学学部灾害风险科学研究院,北京 100875

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强降水 位置偏差 ERA5-Land 中国

国家重点研发计划项目

2020YFA0608201

2024

地理科学
中国科学院 东北地理与农业生态研究所

地理科学

CSTPCDCSSCICHSSCD北大核心
影响因子:3.117
ISSN:1000-0690
年,卷(期):2024.44(10)