The relationship between the monsoon and the temperature is an important part of the global response research to the climate change. Based on the meteorological data of the 56 stations in the Northwestern China from 1961 to 2013, using the trend analysis, Kriging and IDW spatial interpolation method, Mann-Kendall mutation test and Morlet wavelet analysis, this essay analyzes the variation of averaged wind speed of Shandong, Jiangsu, Anhui, Zhejiang Provinces and Shanghai in the East China under the global climate changing from 1961 to 2013. The results show that: (1)The wind speed of Shandong, Jiangsu, Anhui, Zhejiang Provinces and Shanghai is weakening by the rate of 0.013 9 m·s~(-1)· a~(-1) from 1961 to 2013. The wind falls faster in winter, and slower in summer. (2) In the space, the tendency rate of the wind speed exists in zonal distribution, presenting that the decreasing degree is gradually diminishing from central to both ends. (3) The temperature has been rising obviously in the East China from 1961 to 2013, while the wind speed is contrary to the temperature. The wind speed declines quickly after the temperature mutation that happened in 1991. (4) The complex Morlet wavelet analysis reveals that the seasonal wind velocity exhibits quasi-periodic variations of around 28 a. The study on the comprehensive understanding of the relationship between wind speed and the temperature has an important significance. As a whole, the research on the change of the wind speed has a significant importance to the development of the wind resources in the East China.