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首页> 外文期刊>Water Resources Management >Modelling Impacts of Climate Change on a River Basin: Analysis of Uncertainty Using REA & Possibilistic Approach
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Modelling Impacts of Climate Change on a River Basin: Analysis of Uncertainty Using REA & Possibilistic Approach

机译:模拟气候变化对流域的影响:使用REA和可能性方法进行不确定性分析

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摘要

In the context of climate change, the uncertainty associated with Global Climate Models (GCM) and scenarios needs to be assessed for effective management practices and decision-making. The present study focuses on modelling the GCM and scenario uncertainty using Reliability Ensemble Averaging (REA) and possibility theory in projecting streamflows over Wainganga river basin. A macro scale, semi-distributed, grid-based hydrological model is used to project the streamflows from 2020 to 2094. The observed meteorological data are collected from the India Meteorological Department (IMD) and the streamflow data is obtained from Central Water Commission (CWC) Hyderabad. In REA, meteorological data are weighted based on the performance and convergence criteria (GCM uncertainty). Whereas in possibility theory, based on the projection of different GCMs and scenarios during recent past (2006-2015) possibility values are assigned. Based on the possibility values most probable experiment and weighted mean possible CDF for the future periods are obtained. The result shows that there is no significant difference in the outcomes is observed between REA and possibility theory. The uncertainty associated with GCM is more significant than the scenario uncertainty. An increasing trend in the low and medium flows is predicted in annual and monsoon period. However, flows during the non-monsoon season are projected to increase significantly. Moreover, it is observed that streamflow generation not only depends on the change in precipitation but also depends on the previous state of physical characteristics of the region.
机译:在气候变化的背景下,需要评估与全球气候模式(GCM)和情景相关的不确定性,以进行有效的管理实践和决策。本研究的重点是在投影Wainganga流域的水流量时,使用可靠性集合平均(REA)和可能性理论对GCM和情景不确定性进行建模。宏观,半分布式,基于网格的水文模型用于预测2020年至2094年的流量。观测的气象数据是从印度气象局(IMD)收集的,而流量数据是从中央水务委员会(CWC)获得的)海得拉巴。在REA中,根据性能和收敛标准(GCM不确定性)对气象数据进行加权。而在可能​​性理论中,根据近期(2006-2015年)不同GCM和情景的预测,分配了可能性值。基于可能性值,获得了未来期间最可能的实验和加权平均可能的CDF。结果表明,REA和可能性理论之间的结果没有显着差异。与GCM相关的不确定性比情景不确定性更为重要。预计每年和季风期间中低流量会增加。但是,预计非​​季风季节的流量将大大增加。此外,可以观察到,水流的产生不仅取决于降水的变化,而且还取决于该区域的物理特征的先前状态。

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