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《Journal of Glaciology and Geocryology》 2007-01
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Evolvement of the Cumulative Temperatures in China Loess Plateau

WANG Yi-rong1,2 (1.Key Laboratory of Arid Climate Change and Reducing Disaster of Gansu Province,Key Laboratory of Arid Climate Change and Reducing Disaster of China Meteorological Adminstration,Lanzhou Institute of Arid Meteorology,China Meteorological Administration,Lanzhou Gansu 730020,China;2.Lanzhou Regional Climate Center,Lanzhou Gansu 730020,China)  
The China Loess Plateau,about 517 000 km2 in area,is a climatic transition zone from hemi-wetness to hemi-dryness,which is a very sensitive and vulnerable region.By applying empirical orthogonal function(EOF),expanded empirical orthogonal function(EEOF),complex empirical orthogonal function(CEOF),Fractal Dimension and wavelet analysis,the weather data of the plateau from 1961 to 2005 are analyzed in detail,in order to make clear the climatic characteristics of the region,especially,the spatial and temporal variations of cumulative temperatures on the plateau.It is revealed that the cumulative temperatures have good response to climate changes.The cumulative negative temperature had two remarkable phases divided by 1982 and also the cumulative positive temperature had two remarkable phase divided by 1985/1986.By wavelet analysis,3~4 a,7 a and 10~14 a periods are identified in the cumulative negative temperature,and the 3~4 a period was principal.2~4 a,6 a and 10 a periods are identified in the cumulative positive temperature and the 2~4 a period was principal.In the cumulative positive one,after 1985/1986,the 2 a period disappeared,the 4 a period became indistinct,and the 3 a period became distinct.The variation is pronounced in the center plateau.The variation amplitude and the variation signal of the cumulative temperatures decline from the center to the margin of the plateau.The Fractal Dimension of cumulative negative temperature was 0.436 and that of the cumulative positive one was 0.353.The Maximum Fractal Dimension was in the cumulative negative temperature of the China Loess Plateau,of which the reason is that the cumulative negative temperature is more complicated than the cumulative positive temperature in the plateau.It might have something to do with atmosphere circumfluence in summer/winter and the activity of cold or warm air mass.
【Fund】: 国家自然科学基金项目(40675066);; 科技部社会公益研究专项(2004DIB5J196;2005DIB3J100)资助
【CateGory Index】: P461
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