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林榕杰, 方国华, 郭玉雪, 闻 昕.RCP情景下都柳江上游气候变化及径流响应分析水资源与水工程学报[J].,2017,28(1):74-80
RCP情景下都柳江上游气候变化及径流响应分析
Analysis of the climate change and runoff response in Duliu River upper basin under the RCP scenarios
  
DOI:10.11705/j.issn.1672-643X.2017.01.13
中文关键词:  气候变化  径流响应  新安江月水文模型  都柳江流域
英文关键词:climate change  runoff response  monthly hydrological model of Xin'an River  Duliu River basin
基金项目:长江科学院开放研究基金资助项目(CKWV2016370/KY);中央高校基本科研业务费专项资金资助项目(2015B28614); 江苏高校优势学科建设工程资助项目
作者单位
林榕杰, 方国华, 郭玉雪, 闻 昕 (河海大学 水利水电学院江苏 南京 210098) 
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中文摘要:
      建立都柳江上游三水源新安江月水文模型,根据1968-2004年历史降雨、蒸发及径流数据运用遗传算法来率定和优选敏感参数,使用降尺度GCM数据驱动模型得到不同RCP情景下的流域未来月平均径流,并通过线性拟合方法分析都柳江上游未来气象要素及模拟径流过程。结果表明:2020-2099年都柳江年平均降雨基本处于稳定状态,年平均气温和蒸发呈波动增长,局部短时段下降。流域径流流量总体低于历史平均值,年际间波动降低,年内分布不均,主要集中在5-10月份。
英文摘要:
      The monthly generalized model of Xin'an River in three-conponents was established to simulate the rainfall runoff. Where genetic algorithm was used to calibrate and optimize parameters by the historical data of precipitation, evaporation and runoff in the period of 1968 to 2004, then the process of monthly flow of Duliu River upper Basin was predicted by driving the hydrological model from using GCM downscaling data under the various scenarios of RCP. Furthermore, the scenarios of the future climate change and the simulation of hydrogragh in this region were analyzed by using linear regression methods. Results indicate that in the period of 2020 to 2099 the annual precipitation will be presenting a steady tendency, the mean annual temperature and evaporation will show a trend of fluctuation in growth while the locals decline in a short period of time. The total runoff amount in this region will be lower than the historical average level, the interannual fluctuation presents a decreasing tendency and the annual distribution is not symmetrical and mainly distributed from May to October.
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