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基于双重嵌套网格的"8·24"宁夏暴雨成因

白泽贤 蒋云钟 周睿杨 刘晨 杜军凯 李逸凡 陈鑫 汪春光

南水北调与水利科技(中英文)2026,Vol.24Issue(2):406-413,8.
南水北调与水利科技(中英文)2026,Vol.24Issue(2):406-413,8.DOI:10.13476/j.cnki.nsbdqk.2026.0039

基于双重嵌套网格的"8·24"宁夏暴雨成因

Causative mechanisms of the Ningxia"8•24"rainstorm based on a double-nested grid

白泽贤 1蒋云钟 1周睿杨 2刘晨 3杜军凯 1李逸凡 1陈鑫 1汪春光4

作者信息

  • 1. 中国水利水电科学研究院,北京 100038||中国水利水电科学研究院流域水循环模拟与调控国家重点实验室,北京 100078
  • 2. 清华大学,北京 100084
  • 3. 中国水利水电科学研究院流域水循环模拟与调控国家重点实验室,北京 100078||天津科技大学,天津 300457
  • 4. 河北工程大学,河北 邯郸 056038
  • 折叠

摘要

Abstract

This study employs the weather research and forecasting model configured with double-nested grids to simulate an extreme torrential rainfall event over Ningxia from August 24th to 25th,addressing the Ningxia Hui Autonomous Region's lack of real-time monitoring data,which limits research on rainstorm mechanisms.The simulation's accuracy was validated against observations from 25 national meteorological stations.The threat score results are as follows:0.73 for light rain,0.56 for moderate rain,and 0.71 for heavy rain.The study indicates significant regional spatial heterogeneity in precipitation distribution during this short-duration heavy rainfall event.A multi-dimensional analysis that considers atmospheric circulation,moisture transport,and topographic effects was conducted to overcome the limitations of traditional single-factor approaches.The analysis revealed that rainstorm mechanisms involved a coupled system formed between the divergence zone associated with the 200 hPa South Asian high and the ascending branch ahead of the 500 hPa shortwave trough.This system,combined with low-level convergence at 700 hPa,created a distinct"upper-level divergence and low-level convergence"dynamic structure,greatly intensifying vertical ascent.Ningxia was situated in the left-front quadrant of a low-level jet's(LLJ)exit region.The overlap of wind speed and moisture flux convergence supplied abundant moisture transport and enhanced lifting,fueling the rainstorm.Topographic effects on the windward slope of the Helan Mountains triggered intense upward motion and a vertically coherent positive vorticity column extending up to 500 hPa,significantly promoting convection.Conversely,negative vorticity on the leeward slope suppressed precipitation.These findings highlight the crucial influence of topography in regulating the spatial heterogeneity of heavy rainfall.The study concludes that the extreme rainfall event in Ningxia resulted from a complex interaction of atmospheric dynamics,moisture transport,and topographical effects.The coupling of large-scale circulation,localized moisture flux convergence,and orographic lifting played key roles in intensifying convection and precipitation.The results emphasize the need to consider multiple factors when studying extreme weather events,and the findings enhance the understanding of rainfall mechanisms in the region.This research elucidates the multifactor synergy involved in Ningxia rainstorms,aiming to establish a theoretical basis for regional rainstorm forecasting and disaster mitigation.

关键词

宁夏"8·24"暴雨/WRF模式/威胁评分/环流条件/水汽辐合/地形效应

Key words

rainstorm on"8•24"in Ningxia/WRF model/threat score/circulation condition/water vapor condition/topographic effect

分类

建筑与水利

引用本文复制引用

白泽贤,蒋云钟,周睿杨,刘晨,杜军凯,李逸凡,陈鑫,汪春光..基于双重嵌套网格的"8·24"宁夏暴雨成因[J].南水北调与水利科技(中英文),2026,24(2):406-413,8.

基金项目

国家重点研发计划资助项目(2023YFF1304201 ()

2023YFF1304202) ()

国家自然科学基金资助项目(52279030) (52279030)

南水北调与水利科技(中英文)

2096-8086

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