摘要
采用华南沿海气象站气温资料,在排除城市热岛效应的基础上,分析近50年、近100年地表气温的变化趋势,得出华南沿海近51年(1953—2003年)的平均增温速率为0.12℃/10年,近100年(1905—2004年)的增温速率为0.6—0.8℃/100年,均与同时期的北半球(陆地+海面)平均增温速率相近。
Instrumental climatic data from some meteorological observatories of the South China were used to analyze the changing rates of surface air temperatures over last 50 years and 100 years respectively. The impact of anthropogenic greenhouse gas ( or the contribution from urbanization) was removed by comparing to the records from coastal observatories with little human activity influence. The results indicate that the warming rate was 0.12 ℃ /10ys for the period of 1953 -2003, and 0.6 -0.8℃/100ys for the period of 1905 - 2004, which are in agreement with the average land and sea values of Northern Hemisphere at the same period.
出处
《广东气象》
2006年第3期1-5,共5页
Guangdong Meteorology
基金
国家自然科学基金重点项目(40231009)
科技部重大基础研究前期研究专项(2002CCA02700)
关键词
气候学
增温率
回归分析
华南沿海
climatology
warming rate
regression analysis
South China coastal areas