RESOURCES AND ENVIRONMENT IN THE YANGTZE BASIN >> 2017, Vol. 26 >> Issue (06): 937-944.doi: 10.11870/cjlyzyyhj201706016

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SIMULATION AND PROJECTION OF FUTURE CLIMATE CHANGE IN HUBEI PROVINCE USING HIGH-RESOLUTION REGIONAL CLIMATE MODEL

DENG Ting1, WANG Run1,2, JIANG Tong3, HUANG Jin-long4,5, FANG Xiao1, LIU Run1   

  1. 1. College of Resources and Environment, Hubei University, Wuhan 430062, China;
    2. Hubei Key Laboratory of Regional Development and Environmental Response, Wuhan 430062, China;
    3. National Climate Center, China Meteorological Administration, Beijing 100081, China;
    4. State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China;
    5. University of Chinese Academy of Sciences, Beijing 100049, China
  • Received:2016-10-17 Revised:2017-01-12 Online:2017-06-20
  • Supported by:
    CHUTIAN Scholarshop Program

Abstract: Based on the comparative analysis between the simulation data from the high-resolution regional climate model (CCLM) and the CN05.1 data based on the observation in the reference period (1961–2005), we conducted projections on future climate change under the scenario of RCP4.5 at both annual and seasonal scales for the Hubei Province. The results showed:(1)CCLM presented a satisfactory simulation performance on the changing trend of temperature and its spatial distribution pattern, but was not matched very well with the CN05.1 observation precipitation data. (2)Under the RCP4.5, from 2006 to 2050, T, Tmin and Tmax in Hubei Province show a rising trend. The temperature is projected to be rising in all four seasons, while the winter has the fastest increase and the greatest contribution to the rise of annual T, Tmin as well as Tmax. (3)Under the RCP4.5, in the period of 2006–2050, T, Tmin and Tmax will increase in the whole region compared to the reference period. The region with the high increase of temperature is located in the northern part of Hubei section of Han River. In spring, the regions with high increase of temperature are located in northwestern mountain area. In summer, the increase of T, Tmin and Tmax in the middle plain region is higher than other regions. In fall, the increase of T and Tmax in southwestern mountain region is higher than that in other regions. The regions with high increase of Tmin are located in the northern part of Hubei section of Han River. In winter, the increase of T in hilly regions of southeastern Hubei is higher than that in other regions, the same for the Tmin in north part of north section of Han River and Tmax in southwestern mountain region.

Key words: climate model, CCLM, RCP4.5, simulation and projection, Hubei Province

CLC Number: 

  • P463
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