Based on the monthly mean NCEP/NCAR reanalysis dataset and the surface air temperature and precipitation data from 160 China stations, the interannual variations of winter Eurasian teleconnection pattern (EU) and its possible influence on the climate in China are investigated. Wavelet analysis reveals that the significant periods of Eurasian teleconnection pattern index (EU index) are 2－4 years. The result suggests that the interannual variation of the EU is dominant, whereas the interdecadal component is weak. In a winter with positive EU phase, the East Asian westerly jet stream at 200 hPa tends to be enhanced and the East Asian trough at 500 hPa becomes stronger. In the meantime, there are the surface northerly anomalies in East Asia which lead to a cooling condition over there. The opposite situations tend to occur in a negative EU winter. Hence, during the boreal winter the cooling and less precipitation are likely to occur in most of eastern China associated with a positive phase of EU.