Using winter monthly mean temperature data of 39 representative stations in Guizhou from 1962 to 2014, 500 hPa height field data in the Northern Hemisphere and global sea surface temperature (SST) data, temporal and spatial characteristics of winter temperature and their relationships with the 500 hPa height field in the Northern Hemisphere and the global SST field were analyzed by composite analysis, correlation analysis, wavelet analysis and so on.The results show that the winter temperature is about 6.3℃ in Guizhou for recent 53 years, and it appears to be warming up, especially in the northeastern and southwestern edge of the province.The winter temperature is dominated by quasi 7 year and quasi 12 year oscillation.The winter temperature changes suddenly in 1988.The winters are obviously cold before the mutation and warm after the mutation.In abnormal warm winter years, the 500 hPa height anomaly fields are positive at the Greenland, the North American and the middle Pacific, while the rest of regions are negative.The potential height deviation of Eurasia continent is presented as "positive-negative-positive".In abnormal cold winter years, the 500 hPa height fields are positive at the central Siberia region, Western Europe-North Atlantic and the North American, while the rest of regions are negative.In the Eastern Hemisphere, the potential height deviation is presented as "negative-positive-negative" both from west to east and from north to south.The correlation between the winter temperature in Guizhou and the SST in the northeastern Pacific, equatorial eastern Pacific Ocean and the eastern India Ocean in the early autumn is very significant.In the autumn before abnormal warm winter, the sea surface temperature anomaly (SSTA) of the North Pacific (especially the Northwest of Pacific) and the central India Ocean (most significantly) is remarkable.In the autumn before abnormal cold winter, the SSTA of the East and Middle Pacific in the Northern Hemisphere (most significantly) and the Middle India Ocean is obvious.Meanwhile, the SSTA difference center in the anomalous cold and warm winter years is concentrated in the Northeast Pacific and the Middle India Ocean in the Southern Hemisphere.
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