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《Journal of Glaciolgy and Geocryology》 2002-01
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SCL and Decade Change of Climate in East China

LIU Yan-xiang, GAO Xiao-qing (Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou Gansu 730000, China)  
Based on spatial-geomagnetic coupling, air temperature series were simulated and reconstructed by using SCL (sunspot circle length) change and its relation with geomagnetic (on geothermal in this paper) over East China in historic times. Except individual period, the simulative curve is similar as Zhu Kezhen's climatic change curve. The decade change of climate was analyzed in East China over the last {2 500} years, which can reflect the warm-cold change of climate. There are a few disputes in some periods with Zhu's curve, for example, 150~350 A.D. was in a warm and wet period, 1050~1150 A.D. was the Little Climatic Optimum in China, when solar was activity with mean SCL of 8^0~10^0 years, similar to later researcher's result. From Mid-Tang Dynasty to Wudai Dynasty, climate change was unstable with warm-cold alternation. The climate change in the Little Ice Age in East China has been clearly revealed, which can be divided into 3 cold periods and can be sub-divided into 2~3 phases in each period. The result also shows the climate change at present. For example, from the beginning of the 1900s, air temperature was going up to the 1940s, then dropped down to the 1960_1970s, and again increases from the mid-1980s up to now.
【Fund】: 中国科学院知识创新工程重大项目 (KZCX1 10 0 2 );; 国家重点基础研究发展规划项目 (G19980 40 80 0 )资助
【CateGory Index】: P467
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