Future temperature changes over the critical Belt and Road region based on CMIP5 models

Based on data of 22 models from the Coupled Model Inter-comparison Project Phase 5 (CMIP5), the performance of climate simulation is assessed and future changes under RCP2.6, RCP4.5 and RCP8.5 are projected over critical Belt and Road region. Compared with observations, the CMIP5 models simulate the...

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Published inAdvances in climate change research Vol. 9; no. 1; pp. 57 - 65
Main Authors Dong, Tian-Yun, Dong, Wen-Jie, Guo, Yan, Chou, Jie-Ming, Yang, Shi-Li, Tian, Di, Yan, Dong-Dong
Format Journal Article
LanguageEnglish
Published Elsevier B.V 01.03.2018
State Key Laboratory of Earth Surface Processes and Resource Ecology, Beijing Normal University, Beijing 100875, China%School of Atmospheric Sciences, Sun Yat-Sen University, Guangzhou 510275, China
Zhuhai Joint Innovative Center for Climate-Environment-Ecosystem, Future Earth Research Institute, Beijing Normal University, Zhuhai 519087, China%State Key Laboratory of Earth Surface Processes and Resource Ecology, Beijing Normal University, Beijing 100875, China
Zhuhai Joint Innovative Center for Climate-Environment-Ecosystem, Future Earth Research Institute, Beijing Normal University, Zhuhai 519087, China%Business School, Beijing Normal University, Beijing 100875, China%State Key Laboratory of Satellite Ocean Environment Dynamics, Second Institute of Oceanography, Hangzhou, 310012, China
KeAi Communications Co., Ltd
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Summary:Based on data of 22 models from the Coupled Model Inter-comparison Project Phase 5 (CMIP5), the performance of climate simulation is assessed and future changes under RCP2.6, RCP4.5 and RCP8.5 are projected over critical Belt and Road region. Compared with observations, the CMIP5 models simulate the linear trend and spatial distribution of the annual mean surface air temperature (SAT) better in the north (NBR) and south (SBR) of the Belt and Road region. The trend of the 22-model ensemble mean (CMIP5 MME) is 0.70/0.50 °C per 100 years from 1901 to 2005, and the observed trend is 1.11/0.77 °C per 100 years in the NBR/SBR region. After 1971, the relative error between CMIP5 MME and observations is 22%/15% in the NBR/SBR region. Seven/nine models are selected in the NBR/SBR to project future SAT changes under three RCP scenarios. For 2081–2100, warming in the NBR/SBR is projected to be (1.16 ± 0.29)/(0.72 ± 0.32) °C, (2.41 ± 0.54)/(1.55 ± 0.44) °C, and (5.23 ± 1.02)/(3.33 ± 0.65) °C for RCP2.6, RCP4.5, and RCP8.5, respectively. Under the RCP scenarios, the NBR region shows greater warming than the SBR region. The most significant warming is expected in Kazakhstan and the northern part of the SBR. The associated uncertainty generally increases with time under the three RCP scenarios. Furthermore, increases in warming over the Belt and Road region are more remarkable under higher-emission scenarios than lower-emission ones.
ISSN:1674-9278
1674-9278
DOI:10.1016/j.accre.2018.01.003