Performance-Based Evaluation of CMIP5 and CMIP6 Global Climate Models and Their Multi-Model Ensembles to Simulate and Project Seasonal and Annual Climate Variables in the Chungcheong Region of South Korea

被引:3
|
作者
Adelodun, Bashir [1 ,2 ,3 ]
Ahmad, Mirza Junaid [1 ,3 ]
Odey, Golden [1 ]
Adeyi, Qudus [1 ]
Choi, Kyung Sook [1 ,3 ]
机构
[1] Kyungpook Natl Univ, Dept Agr Civil Engn, Daegu 41566, South Korea
[2] Univ Ilorin, Dept Agr & Biosyst Engn, PMB 1515, Ilorin 240003, Nigeria
[3] Kyungpook Natl Univ, Inst Agr Sci & Technol, Daegu 41566, South Korea
关键词
climate change; CMIP5; CMIP6; multi-model ensembles; quantile mapping; performance metrics; statistical techniques; PRECIPITATION; TEMPERATURE; TREND;
D O I
10.3390/atmos14101569
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Extreme climate change events are major causes of devastating impacts on socioeconomic well-being and ecosystem damage. Therefore, understanding the performance of appropriate climate models representing local climate characteristics is critical for future projections. Thus, this study analyses the performance of 24 GCMs from the Coupled Model Intercomparison Project Phases 5 and 6 (CMIP5 and 6) and their multi-model ensembles in simulating climate variables including average rainfall, maximum (Tmax), and minimum (Tmin) temperatures at annual and seasonal scales over the Chungcheong region of South Korea from 1975 to 2015. A trend analysis was conducted to estimate the future trends in climate variables in the 2060s (2021-2060) and 2080s (2061-2100). Inverse distance weighting and quantile delta mapping were applied to bias-correct the GCM data. Further, six major evaluating indices comprising temporal and spatial performance assessments were used, after which a comprehensive GCM ranking was applied. The results showed that CMIP6 models performed better in simulating rainfall, Tmax, and Tmin at both temporal and spatial scales. For CMIP5, the top three performing models were GISS, ACCESS1-3, and MRI-CGCM3 for rain; CanESM2, GISS, and MPI-ESM-L-R for Tmax; and GFDL, MRI-CGCM3, and CanESM2 for Tmin. However, the top three performing models in the CMIP6 were MRI-ESM2-0, BCC_CSM, and GFDL for rain; MIROC6, BCC_CSM, and MRI-ESM2-0 for Tmax, and GFDL, MPI_ESM_HR, and MRI-ESM2-0 for Tmin. The multi-model ensembles (an average of the top three GCMs) performed better in simulating rain and Tmin for both CMIP5 and CMIP6 compared with multi-model ensembles (an average of all the GCMs), which only performed slightly better in simulating Tmax. The trend analysis of future projection indicates an increase in rain, Tmax, and Tmin; however, with distinct changes under similar radiative forcing levels in both CMIP5 and CMIP6 models. The projections under RCP4.5 and RCP8.5 increase more than the SSP2-4.5 and SSP5-8.5 scenarios for most climate conditions but are more pronounced, especially for rain, under RCP8.5 than SSP5-8.5 in the far future (2080s). This study provides insightful findings on selecting appropriate GCMs to generate reliable climate projections for local climate conditions in the Chungcheong region of South Korea.
引用
收藏
页数:26
相关论文
共 50 条
  • [31] Exploring uncertainties in global crop yield projections in a large ensemble of crop models and CMIP5 and CMIP6 climate scenarios
    Müller, Christoph
    Franke, James
    Jägermeyr, Jonas
    Ruane, Alex C.
    Elliott, Joshua
    Moyer, Elisabeth
    Heinke, Jens
    Falloon, Pete D.
    Folberth, Christian
    Francois, Louis
    Hank, Tobias
    Izaurralde, R. César
    Jacquemin, Ingrid
    Liu, Wenfeng
    Olin, Stefan
    Pugh, Thomas A.M.
    Williams, Karina
    Zabel, Florian
    Environmental Research Letters, 2021, 16 (03):
  • [32] Evaluation of the Ability of CMIP6 Global Climate Models to Simulate Precipitation in the Yellow River Basin, China
    Wang, Lin
    Zhang, Jianyun
    Shu, Zhangkang
    Wang, Yan
    Bao, Zhenxin
    Liu, Cuishan
    Zhou, Xiong
    Wang, Guoqing
    FRONTIERS IN EARTH SCIENCE, 2021, 9
  • [33] Using multi-model ensembles of CMIP5 global climate models to reproduce observed monthly rainfall and temperature with machine learning methods in Australia
    Wang, Bin
    Zheng, Lihong
    Liu, De Li
    Ji, Fei
    Clark, Anthony
    Yu, Qiang
    INTERNATIONAL JOURNAL OF CLIMATOLOGY, 2018, 38 (13) : 4891 - 4902
  • [34] Model uncertainties in climate change impacts on Sahel precipitation in ensembles of CMIP5 and CMIP6 simulations (vol 55, pg 1385, 2020)
    Monerie, Paul-Arthur
    Wainwright, Caroline M.
    Sidibe, Moussa
    Akinsanola, Akintomide Afolayan
    CLIMATE DYNAMICS, 2020, 55 (7-8) : 2309 - 2310
  • [35] Performance of CMIP5 wind speed from global climate models for the Bay of Bengal region
    Krishnan, Athira
    Bhaskaran, Prasad K.
    INTERNATIONAL JOURNAL OF CLIMATOLOGY, 2020, 40 (07) : 3398 - 3416
  • [36] Evaluation and bias correction of global climate models in the CMIP5 over the Indian Ocean region
    Mohan, Soumya
    Bhaskaran, Prasad K.
    ENVIRONMENTAL MONITORING AND ASSESSMENT, 2019, 191 (Suppl 3)
  • [37] Evaluation and bias correction of global climate models in the CMIP5 over the Indian Ocean region
    Soumya Mohan
    Prasad K. Bhaskaran
    Environmental Monitoring and Assessment, 2019, 191
  • [38] Reductions in daily continental-scale atmospheric circulation biases between generations of global climate models: CMIP5 to CMIP6
    Cannon, Alex J.
    ENVIRONMENTAL RESEARCH LETTERS, 2020, 15 (06):
  • [39] Evaluating the performance of CMIP3 and CMIP5 global climate models over the north-east Atlantic region
    Jorge Perez
    Melisa Menendez
    Fernando J. Mendez
    Inigo J. Losada
    Climate Dynamics, 2014, 43 : 2663 - 2680
  • [40] Projected future daily characteristics of African precipitation based on global (CMIP5, CMIP6) and regional (CORDEX, CORDEX-CORE) climate models
    Dosio, Alessandro
    Jury, Martin W.
    Almazroui, Mansour
    Ashfaq, Moetasim
    Diallo, Ismaila
    Engelbrecht, Francois A.
    Klutse, Nana A. B.
    Lennard, Christopher
    Pinto, Izidine
    Sylla, Mouhamadou B.
    Tamoffo, Alain T.
    CLIMATE DYNAMICS, 2021, 57 (11-12) : 3135 - 3158