长江流域资源与环境 >> 2021, Vol. 30 >> Issue (3): 614-622.doi: 10.11870/cjlyzyyhj202103009

• 自然资源 • 上一篇    下一篇

RADS数据集在长江上游水库蓄水调度中的应用前景

孙思瑞1,秦鹏程2,陈柯兵3,吴旭树4   

  1. (1. 长江水利委员会水文局长江中游水文水资源勘测局,湖北 武汉 430010; 2. 武汉区域气候中心,湖北 武汉 430074;3. 武汉大学水资源与水电工程科学国家重点实验室,湖北 武汉 430072;4. 华南理工大学土木与交通学院,广东 广州 510641)
  • 出版日期:2021-03-20 发布日期:2021-04-07

Application Prospect of RADS Data Set for Reservoir Impoundment Operation in the Upper Yangtze River

SUN Si-rui 1, QIN Peng-cheng 2, CHEN Ke-bing 3, WU Xu-shu 4   

  1. (1. Middle Changjiang River Bureau of Hydrology and Water Resources Survey,Wuhan 430010,China; 2. Wuhan Regional Climate Center,Wuhan 430074,China; 3. State Key Laboratory of Water Resources and Hydropower Engineering Science,Wuhan University,Wuhan 430072,China; 4. School of Civil Engineering and Transportation, South China University of Technology, Guangzhou 510641, China)
  • Online:2021-03-20 Published:2021-04-07

摘要: 长江上游水库蓄水集中在8~10月,此期正值雨季后期,若水库不能在降水集中的雨季结束前蓄至一定水位,将严重影响水库兴利目标的实现。为优化现有蓄水调度方案,该文选用德州农工大学Rainy And Dry Season(RADS)数据集,长系列的雨季划分资料,分析了长江上游雨季结束时间特征。结果表明,RADS与现有全国、长江上游雨季特征的研究结果较为一致,数据集在研究区域适用性较好。乌江流域的雨季结束时间波动范围明显较大,需重视乌江流域的中长期水文气象预报,以提前预警流域雨季较早结束的情况。而对于乌江、岷江大渡河流域水库联合调度方案所规定的9月1日与10月1日的起蓄时间,1961~2007年中曾出现过雨季更早结束的情况,即对于这两个流域的水库而言,统筹考虑防洪任务与预报水情,蓄水时间可考虑进一步提前。

Abstract: The reservoirs in the Upper Yangtze River are refilled in August-October. This period is in the late rainy season. If a reservoir cannot be refilled at a certain water level before the end of the rainy season when precipitation is concentrated, it will seriously affect the benefits of the reservoir. To optimize the existing reservoir impoundment operation policies, this paper selects the Rainy And Dry Season (RADS) data set of Texas A&M University, and analyzes the characteristics of the rainy season in the Upper Yangtze River. The results show that the characteristics of rainy season for China and the Upper Yangtze River revealed by RADS are similar with those from the existing researches. Thus the data set is applicable in the study area. The demise dates of rainy season in the Wu River Basin fluctuate obviously calling for the medium- and long-term hydrological and meteorological forecast of the Wu River Basin for the warning of the earlier end of the rainy season. For the regulated September 1st and October 1st of reservoirs initial impoundment time in Wu and Min-Dadu Rivers, there were situations that the rainy season ended earlier during 1961-2007. Namely, for reservoirs in the two basins, considering flood prevention tasks and forecasted streamflow conditions, it is necessary to consider further advances the initial impoundment time.

No related articles found!
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
[1] 聂钠, 于坤香. 我国世界自然遗产地旅游业环境经济核算思路[J]. 长江流域资源与环境, 2009, 18(2): 121 .
[2] 宋玉芝,秦伯强, 高光. 附着生物对富营养化水体氮磷的去除效果[J]. 长江流域资源与环境, 2009, 18(2): 180 .
[3] 黄沛生, 刘正文,韩博平. 太湖湖滨带浮叶植物菱(Trapa quadrispinosa Roxb)对氮素再悬浮的影响[J]. 长江流域资源与环境, 2005, 14(6): 750 -753 .
[4] 罗专溪,张 远,郑丙辉,富 国,陆兆华. 三峡水库蓄水初期水生态环境特征分析[J]. 长江流域资源与环境, 2005, 14(6): 781 -784 .
[5] 刘爱霞,刘正军,王 静. 基于PCA变换和神经元网络分类方法的中国森林制图研究[J]. 长江流域资源与环境, 2006, 15(1): 19 -24 .
[6] 蔡邦成,陆根法,宋莉娟,陈克亮. 南水北调东线水源地保护区生态建设的生态经济效益评估[J]. 长江流域资源与环境, 2006, 15(3): 384 -387 .
[7] 王学雷,许厚泽,蔡述明. 长江中下游湿地保护与流域生态管理[J]. 长江流域资源与环境, 2006, 15(5): 564 -568 .
[8] 吕新苗,郑 度. 气候变化对长江源地区高寒草甸生态系统的影响[J]. 长江流域资源与环境, 2006, 15(5): 603 -607 .
[9] 李宽意,刘正文,王春忠,王传海,史加达,胡耀辉. 低溶解氧对苦草生长的影响[J]. 长江流域资源与环境, 2006, 15(5): 670 -673 .
[10] 张 政, 付融冰| 杨海真, 顾国维. 水量衡算条件下人工湿地对有机物的去除[J]. 长江流域资源与环境, 2007, 16(3): 363 .