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Projection of Future Extreme Precipitation and Flood Changes of the Jinsha River Basin in China Based on CMIP5 Climate Models

机译:基于CMIP5气候模式的中国金沙江流域未来极端降水与洪水变化预测。

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摘要

Projecting future changes in extreme flood is critical for risk management. This paper presented an analysis of the implications of the Fifth Coupled Model Intercomparison Project Phase (CMIP5) climate models on the future flood in the Jinsha River Basin (JRB) in Southwest China, using the Xinanjiang (XAJ) hydrologic model. The bias-corrected and resampled results of the multimodel dataset came from the Inter-Sectoral Impact Model Intercomparison Project (ISI-MIP). Relatively optimal general circulation models (GCMs) were selected with probability density functions (PDFs)-based assessment. These GCMs were coupled with the XAJ model to evaluate the impact of climate change on future extreme flood changes in the JRB. Two scenarios were chosen, namely: a midrange mitigation scenario (Representative Concentration Pathway 4.5, RCP4.5) and a high scenario (RCP8.5). Results show that: (1) The XAJ model performed well in simulating daily discharge and was suitable for the study area, with ENS and R2 higher than 0.8; (2) IPSL-CM5A-LR and MIROC-ESM-CHEM showed considerable skill in representing the observed PDFs of extreme precipitation. The average skill scores across the total area of the JRB were 0.41 to 0.66 and 0.53 to 0.67, respectively. Therefore, these two GCMs can be chosen to analyze the changes in extreme precipitation and flood in the future; (3) The average extreme precipitation under 20- and 50-year return period across the JRB were projected to increase by 1.0–33.7% under RCP4.5 and RCP8.5 during 2020 to 2050. The Upper basin is projected to experience the largest increase in extreme precipitation indices, possibly caused by a warmer climate. The extreme flood under 20- and 50-year return period will change by 0.8 to 23.8% and −6.2 to 28.2%, respectively, over this same future period. Most of scenarios projected an increase during the near future periods, implying the JRB would be likely to undergo more flooding in the future.
机译:预测极端洪水的未来变化对于风险管理至关重要。本文利用新安江(XAJ)水文模型,分析了第五次耦合模型比较项目阶段(CMIP5)气候模型对西南金沙江盆地(JRB)未来洪水的影响。多模型数据集的偏差校正和重新采样结果来自部门间影响模型比对项目(ISI-MIP)。通过基于概率密度函数(PDF)的评估选择相对最佳的一般流通模型(GCM)。这些GCM与XAJ模型结合使用,以评估气候变化对JRB未来极端洪水变化的影响。选择了两种方案,即:中型缓解方案(代表浓度途径4.5,RCP4.5)和高方案(RCP8.5)。结果表明:(1)XAJ模型在模拟日排放中表现良好,适用于研究区域,ENS和R 2 均大于0.8; (2)IPSL-CM5A-LR和MIROC-ESM-CHEM在表示观测到的极端降水PDF方面显示出相当的技巧。 JRB整个区域的平均技能得分分别为0.41至0.66和0.53至0.67。因此,可以选择这两个GCM来分析未来极端降水和洪水的变化。 (3)在2020年至2050年期间,在RCP4.5和RCP8.5下,整个JRB在20年和50年回归期的平均极端降水预计将增加1.0-33.7%。上流域预计将经历最大的极端降水指数的增加,可能是由于气候变暖所致。在相同的未来期间,在20年和50年回归期下的极端洪水将分别变化0.8至23.8%和-6.2至28.2%。大多数情况都预计在不久的将来会有增加,这意味着JRB将来可能会遭受更多的洪灾。

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