Changjiang River Scientific Research Institute, Changjiang Water Resources Commission of the Ministry of Water Resources of China; 430010 Wuhan, China.
Int J Environ Res Public Health. 2018 Nov 8;15(11):2491. doi: 10.3390/ijerph15112491.
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 and ² 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.
预测未来极端洪水的变化对于风险管理至关重要。本研究利用新安江(XAJ)水文模型,对中国西南地区金沙江流域(JRB)未来洪水的第五次耦合模式比较计划阶段(CMIP5)气候模型的影响进行了分析。多模式数据集的偏差校正和重采样结果来自部门间影响模型比较计划(ISI-MIP)。利用基于概率密度函数(PDF)的评估方法,选择了相对最优的通用环流模型(GCM)。这些 GCM 与 XAJ 模型耦合,以评估气候变化对 JRB 未来极端洪水变化的影响。选择了两种情景,即:中减排情景(代表性浓度路径 4.5,RCP4.5)和高排放情景(RCP8.5)。结果表明:(1)XAJ 模型在模拟日流量方面表现良好,适用于研究区,和 ²均高于 0.8;(2)IPSL-CM5A-LR 和 MIROC-ESM-CHEM 在表示极端降水观测 PDF 方面具有相当的技能。JRB 总面积的平均技能评分分别为 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 RCP4.5 和 RCP8.5 下,JRB 20 年和 50 年重现期的平均极端降水预计在 2020 年至 2050 年期间将增加 1.0%至 33.7%。上流域预计将经历极端降水指数的最大增长,这可能是由于气候变暖所致。在同一未来时期,20 年和 50 年重现期的极端洪水将分别变化 0.8%至 23.8%和-6.2%至 28.2%。大多数情景预测在近期内会增加,这意味着 JRB 在未来可能会经历更多的洪水。