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山丘区小流域SCS广义单位线产汇流模型

邵嘉佳 李彬权 孟健 任泽凌 黄华平

南水北调与水利科技(中英文)2024,Vol.22Issue(3):618-624,7.
南水北调与水利科技(中英文)2024,Vol.22Issue(3):618-624,7.DOI:10.13476/j.cnki.nsbdqk.2024.0063

山丘区小流域SCS广义单位线产汇流模型

Runoff generation and confluence model coupling SCS-CN and general unit hydrograph for small mountainous watersheds

邵嘉佳 1李彬权 2孟健 3任泽凌 1黄华平4

作者信息

  • 1. 河海大学水文水资源学院,南京 210098
  • 2. 河海大学水文水资源学院,南京 210098||河海大学水安全与水科学协同创新中心,南京 210024
  • 3. 杭州市水文水资源监测中心,杭州 310016
  • 4. 中水珠江规划勘测设计有限公司,广州 510610
  • 折叠

摘要

Abstract

The rainfall generation and confluence in small mountainous watersheds exhibit short and rapid runoff response,characterized by abrupt rises and falls during flood events.The short duration and complexity of flood processes pose challenges for flood forecasting in these regions.Moreover,some remote small mountainous watersheds lack well-equipped monitoring stations,resulting in limited hydrological data availability.These areas are considered to appertain lacking or without data regions,where traditional lumped or distributed hydrological models face limitations.Therefore,it is of great significance to conduct the research on the runoff generation and confluence model in small mountainous watersheds. The improved SCS-CN runoff model and the general unit hydrograph confluence method were coupled,and a case at the upper reaches of the Jiuzhou hydrological station in the Xizhijiang River basin,Pearl River basin,was selected for the validation of the proposed model.The three sources Xin'anjiang model was chosen as a reference model for comparison.The flood relative error(Evol),peak relative error(Epeak),peak occurrence time error(Tlag),and Nash-Sutcliffe efficiency coefficient(Dc)as evaluation indicators for model performance.The applicability of the established runoff model in flood simulation in small mountainous watersheds was examined. Results showed that both models demonstrated the applicability in flood simulation in the study basin,with the Xin'anjiang model exhibiting higher accuracy than the SCS-CN general unit hydrograph model.For all 13 flood events,the Xin'anjiang model produced the average Dc was 0.79,with 10 events meeting all accuracy requirements(|Evol|≤ 20%,[Epeak|≤20%,|Tlag|≤3h,and Dc≥0.6),achieving a pass rate of 77%.Regarding the proposed SCS-CN general unit hydrograph model,the average Dc was 0.70,with 9 events meeting all accuracy requirements,achieving a pass rate of 69%. Overall,the accuracy of the Xin'anjiang model was better than the proposed model in the study basin.However,considering of the newly proposed SCS-CN general unit hydrograph model featured a straightforward structure,with parameters that were easy to determine,and was capable of yielding results with acceptable accuracy.It presented a new modeling option for flood forecasting in small mountainous watersheds.Simultaneously,it also provided support for the research of the regionalization law of parameters in general unit hydrograph model.

关键词

山丘区小流域/新安江模型/SCS模型/广义单位线/洪水预报

Key words

small mountainous watershed/Xin'anjiang model/SCS-CN model/general unit hydrograph/flood forecast

分类

天文与地球科学

引用本文复制引用

邵嘉佳,李彬权,孟健,任泽凌,黄华平..山丘区小流域SCS广义单位线产汇流模型[J].南水北调与水利科技(中英文),2024,22(3):618-624,7.

基金项目

国家重点研发计划项目(2023YFC3209204) (2023YFC3209204)

广州市南沙区水务局重大科技项目(2022-263) (2022-263)

南水北调与水利科技(中英文)

OA北大核心CSTPCD

2096-8086

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