Effects of sunspot cycle length and CO2 on air temperature along Qinghai-Xizang railway and air temperature’s trend prediction

被引:23
作者
Dongliang Li
Hui Guo
Wen Wang
Li Wei
机构
[1] Chinese Academy of Science,Cold & Arid Regions Environmental and Engineering Research Institute
[2] Lanzhou University,Department of Atmospheric Sciences
来源
Science in China Series D: Earth Sciences | 2004年 / 47卷
关键词
Qinghai-Xizang railway; annual mean air temperature; sunspot cycle length (SCL); atmospheric carbon dioxide concentration (CO; ); prediction;
D O I
暂无
中图分类号
学科分类号
摘要
There are well coherences between annual averaged air temperatures at every meteorological station along the Qinghai-Xizang railway, and its 10-year moving average correlation coefficient is 0.92. Thus, the regional averaged annual mean temperature series along the Qinghai-Xizang railway (Trw) from 1935 to 2000 are constructed. The investigation is suggested that: Trw had significant responses to the 5-year lagged sunspot cycle length (SCL) and 15-year lagged concentration of atmospheric carbon dioxide (CO2), and the correlation coefficients between them are -0.76 (SCL) and 0.88 (CO2), respectively. The future SCL is predicted by the model of average generated function constructed with its main cycles of 76a, 93a, 108a, 205a and 275a. The result shows that the SCL would be becoming longer in the first half of the 21st century, and then it could be becoming shorter in the second half of the 21st century. Based on the natural change of SCL and the effect of double CO2 concentration, inrw in the 21st century is forecasted. It could warm up about 0.50°C in the first half of the 21st century compared with the last decade of last century. The mean maximum air temperature could be likely about 0.20°C in July and from 0.40°C to 1.10°C in January. The annual air temperature difference would likely reduce 0.3–1.00°C. The probability of above predictions ranges from 0.64 to 0.73.
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页码:131 / 141
页数:10
相关论文
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  • [1] Gao X.(2003)Numerical Simulation for Influence of Greenhouse Effects on Climatic Change of Qinghai-Xizang Plateau and along Qinghai-Xizang Railway Plateau Meteorology (in Chinese) 22 458-463
  • [2] Li D.(2003)Climatic Change over Qinghai and Xi-zang in 21st Century Plateau Meteorology (in Chinese) 22 451-457
  • [3] Zhao Z.(1955)The sunspot cycle in 649B.C. to A.D. 2000 J. Geophysical Res. 60 127-146
  • [4] Xu Y.(1988)Stable-isotope ratios and concentration of CO Annals of Glaciology 10 1-6
  • [5] Ding Y.(1995) in air from polar ice cores Tellus Series B-Chemical and Physical Meteorology 47 264-272
  • [6] Li D.(1996)CO Journal of Geophysical Research-Atmosphere 101 4115-128
  • [7] Justin S. D.(2000) evolution during the last millennium as recorded by Antarctic and Greenland ice Plateau Meteorology (in Chinese) 19 520-529
  • [8] Siegenthaler U.(2003)Natural and anthropogenic changes in atmospheric CO Plateau Meteorology (in Chinese) 22 440-444
  • [9] Friedli H.(2000) over the last 1000 years from air in Antarctic ice and firn Plateau Meteorology (in Chinese) 19 295-303
  • [10] Loetscher H.(1996)Study of monthly mean air temperature in winter and summer and its abnormal distribution over Qinghai-Xizang Plateau Science in China, Series D (in Chinese) 26 348-353