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

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 regionality 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.