The Fractal Dimension Distribution of the Short-Term Climate System in China and It's Connection with the Monsoon Climate  

作　　者：张福青 林振山 蒋全荣 

机构地区：[1]Department of Atmospheric Sciences, Nanjing University, Nanjing 210008

出　　处：《Advances in Atmospheric Sciences》1994年第4期459-462,共4页大气科学进展（英文版）

基　　金：This work is supported by both NKPFR and NNSF of China.

摘　　要： By analyzing the Fractal Dimension(FD) distribution of the Short-range Climate system(SCS) in China, it is found that the FD varies in different region and this just agrees with the regionally of the monsoon climate in China. The FD of the SCS Lays between 2.0 and 5.0. In the vast eastern area of China, the FD almost grows gradually with the latitude. Line 4.0 is along the mountain chains from the Nanlin Mountain to the Wuyi Mountain. North of the line the FD varies only slightly and all are above 4.0. Only in coastal islands the FD is smaller than 3.0.By analyzing the Fractal Dimension(FD) distribution of the Short-range Climate system(SCS) in China, it is found that the FD varies in different region and this just agrees with the regionally of the monsoon climate in China. The FD of the SCS Lays between 2.0 and 5.0. In the vast eastern area of China, the FD almost grows gradually with the latitude. Line 4.0 is along the mountain chains from the Nanlin Mountain to the Wuyi Mountain. North of the line the FD varies only slightly and all are above 4.0. Only in coastal islands the FD is smaller than 3.0.

关 键 词：Short-range Climate System(SCS) Fractal Dimension(FD) Monsoon climate Climate division 

分 类 号：P461[天文地球—大气科学及气象学]