首页|结合DEM的短时强降水空间分布特征分析——以广州市为例

结合DEM的短时强降水空间分布特征分析——以广州市为例

扫码查看
利用广州市2014-2023年316个自动气象站逐时降水数据对近10年短时强降水频次进行统计,引入数字高程模型,运用协同克里金空间插值法,对不同时间尺度的短时强降水频次空间分布特征进行深入分析.结果表明:广州市短时强降水呈现中东部多、西部和南部相对较少的特征,有4个高发中心;前汛期短时强降水频次和范围均高于后汛期;4-6月广州北部和东部山地、丘陵地区短时强降水频发,7-8月呈现局地散发特征,9月中心城区频发;广州中南部地区在早晨至中午最易出现短时强降水,中北部丘陵地带则多发于夜间.
Analysis of spatial distribution characteristics of short-term heavy rainfall combined with DEM Taking Guangzhou City as an axample
Based on the hourly precipitation data of 316 automatic meteorological observation stations in Guangzhou from 2014 to 2023,the frequency of short-term heavy rainfall(STHR)in recent 10 years was analyzed.A Digital Elevation Model(DEM)was introduced,and the Collaborative Kriging(COK)spatial interpolation method was used to conduct in-depth analysis of the spatial distribution characteristics of STHR frequency at different time scales.The results show that the STHR in Guangzhou is more in the eastern part of the city,less in the western and southern part,with 4 high incidence centers.The frequency and range of STHR in the pre-flood season were higher than those in the post-flood season.From April to June,STHR occurred frequently in the mountainous and hilly areas in the north and east of Guangzhou,with local distribution characteristics in July to August and frequent occurrence in the central urban area in September.The central and southern parts of Guangzhou are most prone to STHR in the morning to noon,while the hilly areas in the central and northern parts tend to occur at night.

short-term heavy rainfallspatial distributionDigital Elevation ModelCollaborative Kriging

问楠臻、焦玚、蔡顺明、朱丽媛、伍瑞林、何耀斌

展开 >

广州市荔湾区气象局,广州 510150

广州市气象台,广州 511430

短时强降水 空间分布 数字高程模型 协同克里金

广州市科技计划基础与应用基础研究专项

2023A04J1546

2024

气象水文海洋仪器
中国仪器仪表学会 气象水文海洋仪器分会 长春气象仪器研究所

气象水文海洋仪器

影响因子:0.307
ISSN:1006-009X
年,卷(期):2024.41(2)
  • 12