主办单位:中国气象局沈阳大气环境研究所
国际刊号:ISSN 1673-503X
国内刊号:CN 21-1531/P

Journal of Meteorology and Environment ›› 2018, Vol. 34 ›› Issue (6): 56-63.doi: 10.3969/j.issn.1673-503X.2018.06.006

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Projection of surface wind by CMIP5 and CMIP3 in China in the 21st century

JIANG Ying1, XU Xi-yan2, LIU Han-wu3, WANG Wen-ben3, DONG Xu-guang4   

  1. 1. Specialized Meteorological Office of CMA Public Meteorological Service Center, Beijing 100081, China;
    2. CAS Key Laboratory of Regional Climate-Environment for Temperate East Asia, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China;
    3. Meteorological Service of Chaohu Lake Basin, Hefei 238000, China;
    4. Shandong Climate Center, Ji'nan 250031, China
  • Received:2017-07-17 Revised:2017-11-27 Online:2018-12-31 Published:2018-12-31

Abstract: The change of surface wind speed was projected by 23 Climate models from the CMIP5 (Coupled Model Intercomparison Project Phase 5) for IPCC AR5 (Intergovernmental Panel on Climate Change Fifth Assessment Report) adapted by WCRP (Word Climate Research Programme) and 19 Climate models from the CMIP3 (Coupled Model Intercomparison Phase 3) for IPCC AR4 (Intergovernmental Panel on Climate Change Fourth Assessment Report) adapted by WCRP (Word Climate Research Programme).The human emission scenarios used the RCPs (Representative Concentration Pathways) including RCP2.6,RCP4.5 RCP8.5 from CMIP5 and the SRES (Special Report on Emissions Scenarios) including B1,A1B,A2 from CMIP3.The results show that the mean annual wind speeds would decrease slightly in China in the 21st century.The mean wind speeds would reduce more significantly with the increase of human emission concentration.Both CMIP5 and CMIP3 project that the mean annual wind speed in Western China (Northern and Southwestern parts) would decrease in the 21st Century and would increase in the eastern region.Compared with that in the early period of the 21st Century (2006-2015),wind speed would decrease in the south of Northeast China,north of North China and West China,while it would increase in the south of North China,South China and the north of Northeast China in the late 21st Century (2090-2099).With the increase of human emission concentration,the negative (positive) deviation ranges in wind would enlarge and the corresponding center value would be more concentrated in winter (summer).

Key words: CMIP5, CMIP3, Surface wind speed, RCP, Projection

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