院报 ›› 2021, Vol. 38 ›› Issue (8): 25-32.DOI: 10.11988/ckyyb.20200659

• 水资源 • 上一篇    下一篇

基于试验流域的季风区洪水特性及其水文模拟

刘悦1,2,3,4, 张建云1,2,3,4, 陈鑫2,3, 王婕2,3, 鲍振鑫2,3, 管晓祥1,2,3,4, 刘翠善2,3, 王国庆2,3,4   

  1. 1.河海大学 水文水资源学院, 南京 210098;
    2.水利部应对气候变化研究中心, 南京 210029;
    3.长江保护与绿色发展研究院,南京 210098;
    4.南京水利科学研究院 水文水资源与水利工程科学国家重点实验室, 南京 210029
  • 收稿日期:2020-07-03 修回日期:2020-10-10 出版日期:2021-08-01 发布日期:2021-08-06
  • 通讯作者: 王国庆(1971-),男,山东成武人,教授级高级工程师,博士,从事气候变化和水资源评价方面的研究。E-mail:gqwang@nhri.cn
  • 作者简介:刘 悦(1996-),女,江苏盐城人,博士研究生,研究方向为水文水资源模拟。E-mail:liuyue_hhu@163.com
  • 基金资助:
    国家自然科学基金项目(41830863, 51879162)

Flood Characteristics and Hydrological Simulations in Monsoon Area Based on Experimental Watersheds

LIU Yue1,2,3,4, ZHANG Jian-yun1,2,3,4, CHEN Xin2,3, WANG Jie2,3, BAO Zhen-xin2,3, GUAN Xiao-xiang1,2,3,4, LIU Cui-shan2,3, WANG Guo-qing2,3,4   

  1. 1. College of Hydrology and Water Resource, Hohai University, Nanjing 210098, China;
    2. Research Center of Climate Change, Ministry of Water Resources, Nanjing 210029, China;
    3. Yangtze Institute for Conservation and Development, Nanjing 210098, China;
    4. State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Nanjing Hydraulic Research Institute, Nanjing 210029, China
  • Received:2020-07-03 Revised:2020-10-10 Online:2021-08-01 Published:2021-08-06

摘要: 根据我国安徽省5个试验流域的实测资料,分析了各流域场次洪水的特性,并利用TOPMODEL模型对各流域进行次洪模拟,进一步探讨该模型在我国东部季风区洪水预报方面的适用性。结果表明:安徽省各试验流域场次洪水的降雨量-径流深散点均呈现较好的正相关性,降雨量随着海拔的升高而增大,山区的径流系数大于平原丘陵区;面积最小的瓦屋刘流域对暴雨的响应最为敏感,孙村流域场次洪水的洪峰模数差异最小、起涨时间最长,黄山流域场次洪水的历时最久;随着海拔的升高,流域地形指数的平均值逐渐增大,同时各流域面积占比最大所对应的地形指数逐渐减小;地形指数标准差越大的流域,土地利用类型也越丰富;TOPMODEL模型总体上可以较好地模拟安徽省各试验流域场次洪水过程,且对大流量的捕捉效果优于小流量,对天然流域的模拟效果优于人类活动扰动的流域。

关键词: 洪水特性, 地形指数, 试验流域, TOPMODEL模型, 次洪模拟

Abstract: Study on flood characteristics and hydrological simulations are of great significance to flood control and disaster mitigation. According to the measured data of five experimental watersheds in Anhui Province, we analyze the characteristics of the floods in each watershed, and then simulate the floods in each watershed by using TOPMODEL to examine its applicability in flood forecasting in the monsoon region of east China. Our results reveal that the rainfall-runoff scatter points of floods in each experimental watershed all present a good positive correlation. The rainfall amount increases with the rising of elevation, and the runoff coefficients in mountainous area are greater than those in the plain and hilly area. The Wawuliu watershed which has the smallest area is the most sensitive to storms; the Suncun watershed features the smallest difference in the modulus of flood peak and the longest flood rising time; while the Huangshan watershed has the longest flood duration. The average value of watershed's topographic index gradually increases with the rising of altitude, while the value corresponding to the largest proportion drops. And the larger the standard deviation of the topographic index is, the more diversified land use types the watershed has. The TOPMODEL can generally reproduce the flood processes of each experimental watershed, and the captured results of large flows are better than those of small ones. The simulation of natural watersheds is better than that of human-disturbed watersheds.

Key words: flood characteristics, topographic index, experimental watersheds, TOPMODEL, flood simulations

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