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Impact of Climate Change on the Hydrology of Upper Tiber River Basin Using Bias Corrected Regional Climate Model

机译:偏差校正的区域气候模型对气候变化对台伯河上游水文学的影响

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摘要

The use of regional climate model (RCM) outputs has been getting due attention in most European River basins because of the availability of large number of the models and modelling institutes in the continent; and the relative robustness the models to represent local climate. This paper presents the hydrological responses to climate change in the Upper Tiber River basin (Central Italy) using bias corrected daily regional climate model outputs. The hydrological analysis include both control (1961-1990) and future (2071-2100) climate scenarios. Three RCMs (RegCM, RCAO, and PROMES) that were forced by the same lateral boundary condition under A2 and B2 emission scenarios were used in this study. The projected climate variables from bias corrected models have shown that the precipitation and temperature tends to decrease and increase in summer season, respectively. The impact of climate change on the hydrology of the river basin was predicted using physically based Soil and Water Assessment Tool (SWAT). The SWAT model was first calibrated and validated using observed datasets at the sub-basin outlet. A total of six simulations were performed under each scenario and RCM combinations. The simulated result indicated that there is a significant annual and seasonal change in the hydrological water balance components. The annual water balance of the study area showed a decrease in surface runoff, aquifer recharge and total basin water yield under A2 scenario for RegCM and RCAO RCMs and an increase in PROMES RCM under B2 scenario. The overall hydrological behaviour of the basin indicated that there will be a reduction of water yield in the basin due to projected changes in temperature and precipitation. The changes in all other hydrological components are in agreement with the change in projected precipitation and temperature.
机译:由于欧洲大陆上有大量的模型和建模机构,在大多数欧洲河流域,使用区域气候模型(RCM)的输出已引起了应有的重视;和代表模型的相对鲁棒性。本文利用偏差校正的每日区域气候模型输出结果,展示了上台伯河流域(意大利中部)对气候变化的水文响应。水文分析包括控制(1961-1990年)和未来(2071-2100年)气候情景。在本研究中,使用了在相同的横向边界条件下在A2和B2排放情景下施加的三个RCM(RegCM,RCAO和PROMES)。来自偏差校正模型的预计气候变量显示,夏季降水和温度分别趋于下降和升高。使用基于物理的土壤和水评估工具(SWAT)预测了气候变化对流域水文学的影响。首先使用子盆地出口处的观测数据集对SWAT模型进行校准和验证。在每种情况和RCM组合下总共进行了六次仿真。模拟结果表明,水文水平衡要素存在明显的年度和季节变化。在RegCM和RCAO RCM的A2方案下,研究区域的年度水平衡显示出地表径流量,含水层补给和流域总水减少,在B2方案下,PROMES RCM有所增加。流域的整体水文行为表明,由于预计的温度和降水变化,流域的水产量将减少。所有其他水文要素的变化与预计降水量和温度的变化一致。

著录项

  • 来源
    《Water Resources Management》 |2014年第5期|1327-1343|共17页
  • 作者单位

    Dipartimcnto di Scienze dell'Ingegneria Civile, Universita di Roma Tre, Rome, Italy Department of Earth and Environment, Florida International University, Miami, FL 33199, USA;

    Department of Earth and Environment, Florida International University, Miami, FL 33199, USA;

    Department of Earth and Environment, Florida International University, Miami, FL 33199, USA;

    Dipartimcnto di Scienze dell'Ingegneria Civile, Universita di Roma Tre, Rome, Italy;

    Dipartimcnto di Scienze dell'Ingegneria Civile, Universita di Roma Tre, Rome, Italy;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    RCM; Bias correction; Climate change; Hydrological modeling; SWAT; Tiber River basin;

    机译:RCM;偏差校正;气候变化;水文模拟;扑打;台伯河流域;

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