Assessment of Nonstationarity and Uncertainty in Precipitation Extremes of a River Basin Under Climate Change

被引:0
作者
S. Ansa Thasneem
N. R. Chithra
Santosh G. Thampi
机构
[1] National Institute of Technology Calicut,Department of Civil Engineering
来源
Environmental Modeling & Assessment | 2021年 / 26卷
关键词
Climate change; Nonstationarity; Extreme precipitation; Uncertainty;
D O I
暂无
中图分类号
学科分类号
摘要
In this study, an uncertainty analysis of extreme precipitation return levels was performed for the Chaliyar river basin, India, under representative concentration pathways (RCPs) 4.5 and 8.5. Weighted average projections of various climate models (for RCPs 4.5 and 8.5) using reliability ensemble averaging were used in the analysis for projecting the future extremes. To start with, the presence of nonstationarity in the observed annual maximum precipitation (AMP) series and the future ensemble averaged AMP projections were investigated. For this purpose, three generalized extreme value (GEV) models—one stationary model with constant parameters and two nonstationary models with trends in location and scale parameters—were applied to assess the goodness of fit using Akaike information criterion and likelihood ratio test. The best fit model was used in the uncertainty analysis, and the confidence bounds of extreme precipitation return levels were estimated. A nonparametric bootstrapping approach was followed in the uncertainty analysis. Results of the study suggest that a nonstationary GEV distribution with linear trend in location parameter and constant scale and shape parameters are the best fit distribution for the AMP series under the RCP scenarios, whereas the stationary GEV distribution fits the observed AMP series the best. The expected values and confidence bounds of return levels obtained from the uncertainty analysis reveal that precipitation extremes in the river basin would intensify under the projected climate change scenarios. Compared with the RCP4.5 scenario, the confidence intervals of return levels under the RCP8.5 scenario were wider, implying that uncertainty in the latter scenario is higher.
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页码:295 / 312
页数:17
相关论文
共 244 条
[1]  
Trenberth KE(1998)Atmospheric moisture residence times and cycling: Implications for rainfall rates and climate change Climatic Change 39 667-694
[2]  
Muller CJ(2011)Intensification of precipitation extremes with warming in a cloud-resolving model Journal of Climate 24 2784-2800
[3]  
O’Gorman PA(2000)Climate extremes: observations, modeling, and impacts Science 289 2068-2074
[4]  
Back LE(2001)Detection probability of trends in rare events: Theory and application to heavy precipitation in the Alpine region Journal of Climate 14 1568-1584
[5]  
Easterling DR(2006)Increasing trend of extreme rain events over India in a warming environment Science 314 1442-1445
[6]  
Meehl GA(2003)Trends in extreme daily rainfall across the South Pacific and relationship to the South Pacific convergence zone International Journal of Climatology 23 847-869
[7]  
Parmesan C(2000)Trends in extreme rainfall indices for an updated high quality data set for Australia, 1910–1998 International Journal of Climatology 20 1533-1615
[8]  
Changnon SA(2001)Trends in New Zealand daily temperature and rainfall extremes International Journal of Climatology 21 1437-1452
[9]  
Karl TR(2018)The Kerala flood of 2018: combined impact of extreme rainfall and reservoir storage Hydrology and Earth System Sciences Discussions 1–13 2018-53
[10]  
Mearns LO(2018)Increase in extreme precipitation events under anthropogenic warming in India Weather and Climate Extremes 20 45-171