Performance evaluations of CMIP6 and CMIP5 models for precipitation simulation over the Hanjiang River Basin, China

被引:7
|
作者
Wang, Dong [1 ,2 ]
Liu, Jiahong [2 ]
Wang, Hao [1 ,2 ]
Shao, Weiwei [2 ]
Mei, Chao [2 ]
Ding, Xiangyi [2 ]
机构
[1] Jilin Univ, Coll New Energy & Environm, Changchun 130021, Jilin, Peoples R China
[2] China Inst Water Resources & Hydropower Res, State Key Lab Simulat & Regulat Water Cycle River, Beijing 100038, Peoples R China
基金
中国国家自然科学基金;
关键词
CMIP5; CMIP6; GCM; Hanjiang River Basin; precipitation simulation performance; SUMMER MONSOON; CLIMATE-CHANGE; TEMPERATURE; MANAGEMENT; SYSTEM; REGION;
D O I
10.2166/wcc.2022.402
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
Projecting the climate change impacts on the hydrology and water resources relies on the climate scenarios simulated by general circulation models (GCMs), which requires a systematic and comprehensive assessment of the GCMs' simulation performances at a regional scale. This study evaluates the performances of precipitation simulation over the Hanjiang River Basin (HRB) by six climate models from the Phase 6 of the Coupled Model Intercomparison Project (CMIP6), the corresponding six previous models from the CMIP5, and their multi-model ensemble (MME) based on the observational data in the CN05.1. To our knowledge, this is the first preliminary study in the HRB. The Taylor diagram (including standard deviation, root-mean-square difference, and correlation coefficient) and Taylor skill score are used for the evaluation of GCMs' precipitation simulation performances. The spatial pattern and temporal pattern over the HRB simulated by CMIP6 and CMIP5 models are compared by relative biases. The results of the Taylor diagram and skill score show that CMIP6 models don't necessarily perform better than the corresponding previous CMIP5 models in simulating precipitation over the HRB. The MME exhibits superior performance than that of any individual model, and the CMIP6-MME is more skillful than the CMIP5-MME. As to the spatial and temporal variation characteristics, the precipitation biases are both present in CMIP6 and CMIP5 models, and the bias of the CMIP6-MME is lower than that of the CMIP5-MME. The CMIP6 and CMIP5 models overestimate the precipitation from January to June, and simulate larger precipitation biases in the areas and seasons with less precipitation, while lower with more precipitation over the HRB. The findings obtained in this study could provide a scientific reference for the research of future hydrological cycle predictions over the HRB.
引用
收藏
页码:2089 / 2106
页数:18
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