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DOI | 10.1007/s00382-019-04860-8 |
Drylands climate response to transient and stabilized 2 °C and 1.5 °C global warming targets | |
Wei Y.; Yu H.; Huang J.; Zhou T.; Zhang M.; Ren Y. | |
发表日期 | 2019 |
ISSN | 0930-7575 |
起始页码 | 2375 |
结束页码 | 2389 |
卷号 | 53期号:2020-03-04 |
英文摘要 | Drylands are one of the most sensitive areas to climate change. Many previous studies assessed the impact of 1.5 °C and 2 °C warming targets using transient warming scenarios by representative concentration pathways of CMIP5. Here we compared the climate changes over global drylands in transient and stabilized 1.5 °C and 2 °C warmer worlds using Community Earth System Model simulations. The projections indicate a warming of 2.3 °C (1.6 °C) over drylands could occur in a stabilized 2 °C (1.5 °C) warmer world by the end of this century. The warming in drier regions is higher and the hyper-arid areas would experience warming of 2.4 °C (1.8 °C). Comparing the 2 °C to 1.5 °C warming targets, the additional 0.5 °C warming will lead to ~ 1.0 °C warming in drylands of Eurasia and North America. Responding to the 2 °C warming, the increased precipitation (21.8–42.6 mm/year) is not enough to offset the increased PET (88.3–101.7 mm/year) over drylands, resulting in the drylands expansion, and the additional 0.5 °C global warming will aggravate the drought in drylands in southern North America and North Africa. Compared to the stabilized 2 °C warming target, controlling the global warming to within 1.5 °C will reduce the warming in drylands by 0.7 °C, and reduce the drylands expansion relative to 1961–1990 by ~ 44%. Compared to the stabilized warming scenarios, the temperature response and drylands area coverage increase are higher in the transient warming scenarios, but the difference of temperature caused by additional 0.5 °C global warming and the precipitation increase in drylands are lower. © 2019, Springer-Verlag GmbH Germany, part of Springer Nature. |
英文关键词 | 1.5 °C and 2 °C warming target; Drylands climate change; The Paris Agreement; Transient and stabilized warming world |
语种 | 英语 |
scopus关键词 | climate modeling; drought; global warming; high temperature; regional climate; temperature profile; Eurasia; North Africa; North America |
来源期刊 | Climate Dynamics
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/146095 |
作者单位 | Key Laboratory for Semi-Arid Climate Change of the Ministry of Education, College of Atmospheric Sciences, Lanzhou University, Lanzhou, 730000, China; Key Laboratory of Arid Climate Change and Reducing Disaster of Gansu Province, Key Open Laboratory of Arid Climate Change and Disaster Reduction of CMA, Institute of Arid Meteorology, China Meteorological Administration, Lanzhou, 730020, China; State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, 100029, China; College of Earth Sciences, University of Chinese Academy of Sciences, Beijing, 100049, China |
推荐引用方式 GB/T 7714 | Wei Y.,Yu H.,Huang J.,et al. Drylands climate response to transient and stabilized 2 °C and 1.5 °C global warming targets[J],2019,53(2020-03-04). |
APA | Wei Y.,Yu H.,Huang J.,Zhou T.,Zhang M.,&Ren Y..(2019).Drylands climate response to transient and stabilized 2 °C and 1.5 °C global warming targets.Climate Dynamics,53(2020-03-04). |
MLA | Wei Y.,et al."Drylands climate response to transient and stabilized 2 °C and 1.5 °C global warming targets".Climate Dynamics 53.2020-03-04(2019). |
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