首页|海河"23·7"流域性特大洪水复盘模拟

海河"23·7"流域性特大洪水复盘模拟

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为支撑海河流域特大洪水的决策及预报预警工作,基于实测降水与流量资料,采用新安江-海河模型对海河流域2023年7月发生特大洪水的大清河2个典型小流域——紫荆关流域和漫水河流域进行了洪水模拟,并选取紫荆关流域1996-2020年5场洪水、漫水河流域1953-2016年8场洪水进行了参数率定,选取海河"23·7"流域性特大洪水进行了验证.结果表明:新安江-海河模型对"23·7"流域性特大洪水的模拟精度较高,可反映实际洪水过程,两个小流域洪峰、洪量模拟的相对误差均在20%以内,峰现时间误差均为0 h;相较于受人类活动影响小的紫荆关流域,在受人类活动影响更大的漫水河流域,新安江-海河模型的模拟效果较新安江模型的模拟效果提升更为明显.
Retrospective simulation on the Haihe"23·7"basin-wide extreme flood
To support the decision-making and forecasting work for the catastrophic flood in the Haihe River Basin,the Zijingguan and Manshuihe sub-basins,located in the Daqing River where a catastrophic flood occurred in July 2023,were selected for the flood simulation and prediction with the Xin'anjiang-Haihe model based on measured rainfall and discharge data.For the Zijingguan sub-basin,5 floods from 1996 to 2020 were chosen for the parameter calibration,while for the Manshuihe sub-basin,8 floods from 1953 to 2016 were used.The simulation was validated against the Haihe"23·7"basin-wide extreme flood event.The results showed that the relative errors of peak discharge and flood volume in both sub-basins were within 20%,with a peak timing error of 0 hours.The high accuracy of the hydrological model constructed in this study,along with the good agreement between simulation and measured results,demonstrates its ability to reflect the actual flood process.A comparison between different models revealed that the Xin'anjiang-Haihe model performed better in the Manshuihe sub-basin,which is more affected by human activities,compared to the Zijingguan sub-basin with lesser human influence.

Haihe"23·7"basin-wide extreme floodextreme precipitationflood forecastingXin'anjiang-Haihe modelhydrological model

李致家、张心愿、白云鹏、黄鹏年

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河海大学水文水资源学院,江苏南京 210098

河北省水文勘测研究中心,河北石家庄 050031

南京信息工程大学水文与水资源工程学院,江苏南京 210044

水利部水文气象灾害机理与预警重点实验室,江苏南京 210044

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海河"23·7"流域性特大洪水 极端降水 洪水预报 新安江-海河模型 水文模型

国家自然科学基金项目河北省水利厅科技项目

520790352022-40

2024

河海大学学报(自然科学版)
河海大学

河海大学学报(自然科学版)

CSTPCD北大核心
影响因子:0.803
ISSN:1000-1980
年,卷(期):2024.52(5)