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| The Relationship Between Early Summer Air Temperature and the Global Sea Surface Temperature in the North of Western Sichuan Plateau from 1854 to 2010 |
| Li Jinjian1,2, Shao Xuemei3, Li Yuanyuan1,2, Qin Ningsheng1,2, Yang Tao4 |
1. Chengdu Institute of Plateau Meteorology, China Meteorological Administration, Chengdu 610072, China;
2. Agrometeorological Center of Sichuan Province, Chengdu 610072, China;
3. Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China;
4. Sichuan Technical Center for Atmospheric Sounding, Chengdu 610072, China |
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Abstract In this paper, five tree-ring chronologies from the north of Western Sichuan Plateau were analyzed for regional common information by using the principal component analysis (PCA) method. The variance contribution of first principal component (PC1) is 59.52%, which could represent the most common features about the tree-ring variations of north of Western Sichuan Plateau. During 1961-2010, the spatial correlation between meteorological records and PC1 chronology with CRU data were calculated. The result suggested the PC1 could represent air temperature variation in larger scale, and positively correlated with that in Northwestern China-Tibet Plateau and Eastern Siberia(r>0.443, p<0.001). The PC1 and meteorological records were used to investigate the influence of global SST on the regional temperature variability during the modern instrumental observation period (1961-2010), the coincident significant positive correlation were observed for the Western Pacific, the Equatorial Indian Ocean, the South Subtropical Indian Ocean, the Equatorial Atlantic and the North Atlantic. It indicated that the change of multiple ocean sea surface temperature could effect on which is in the studied area. However, by the using the PC1 chronology in the longer time scale (1854-2010) and phased analysis found the obvious differences of different stages on the temperature leading regional sea, and even opposite distribution patterns exist in different stages in larger space.The correlation coefficient of the intensity of the air-sea interaction has significant difference. When the temperatures fluctuation was severer, the air-sea interaction was more intense. The results of abnormal analysis suggest that the influence of the northwestern Pacific and northern Atlantic SST are stable and sustained.
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Received: 31 July 2014
Published: 20 July 2015
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2015, Vol. 35 
