Deciphering the projected changes in CMIP-6 based precipitation simulations over the Krishna River Basin

被引:13
作者
Anil, Suram [1 ]
Raj, Anand P. [1 ]
机构
[1] Natl Inst Technol Warangal, Dept Civil Engn, Hanamkonda 506004, Telangana, India
关键词
global circulation models; Krishna River Basin; precipitation projection; reliable ensemble average; shared socioeconomic pathways; symmetric uncertainty; CLIMATE-CHANGE IMPACT; GENERAL-CIRCULATION MODELS; MULTIMODEL ENSEMBLE; MINIMUM TEMPERATURE; FEATURE-SELECTION; MAXIMUM TEMPERATURE; RAINFALL; INDIA; PERFORMANCE; GCM;
D O I
10.2166/wcc.2022.399
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
The impact of climate change on the Krishna River Basin (KRB) is significant due to the semi-arid nature of the basin. Herein, 21 global climate models (GCMs) of Coupled Model Intercomparison Project Phase 6 (CMIP6) were examined to simulate the historical monthly precipitation over the 1951-2014 period in the KRB. The symmetrical uncertainty (SU) method and the multi-criteria decision method (MCDM) were employed to select the suitable GCMs for projecting possible changes in precipitation over the KRB. The biases in the climate projections were removed by using the empirical quantile mapping method. The reliability ensemble averaging (REA) method was used to generate the multi-model ensemble (MME) mean of projections and to analyse the spatio-temporal changes of precipitation under different shared socioeconomic pathways (SSPs). BCC-CSM2-MR, IPSL-CM6A-LR, MIROC6, INM-CM5-0, and MPI-ESM1-2-HR were found to be the most suitable GCMs for the KRB. The MME mean of the chosen GCMs showed significant changes in precipitation projection that occurs for a far future period (2071-2100) over the KRB. The projection changes of precipitation range from -36.72 to 83.05% and -37.68 to 95.75% for the annual and monsoon periods, respectively, for various SSP5. Monsoon climate projections show higher changes compared with the annual climate projections, which reveals that precipitation concentration is more during the monsoon period over the KRB.
引用
收藏
页码:1389 / 1407
页数:19
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