Dynamics of vegetation change on different spatial and temporal scales in Mongolia were analysed for the period from 1982 to 2015, based on GIMMS NDVI3g data (global inventory monitoring and modeling system normalized difference vegetation index-3rd generation), climate data, and data on vegetation type from 1982 to 2015. Spatial patterns, trends of change in those patterns, and the main reasons for differences in vegetation type were examined using trend analysis, partial correlation analysis and residual analysis. The average NDVI in Mongolia in the growing season increased gradually from the south to the north across Mongolia over the 34-year period, showed significant latitudinal differences, and decreased as the altitude increased. In the growing season, the NDVI displayed characteristic features in particular time periods, notably a significant increase between 1982 and 1994 and between 2007 and 2015, and a significant decrease between 1994 and 2007. Across the whole of Mongolia, linear regression model indicated an increasing trend in the values of the NDVI during the growing season at the rate of 0.0005 NDVI per year, and changes in the index were closely related to increasing precipitation, with a partial correlation coefficient of 0.74. In the case of spatial distribution, areas with significant increase in vegetation were distributed mainly in the Great Lakes Region in the west, the Hangayn Mountains, the Gobi Altai Mountains, and the northern forest areas. The responses of vegetation to climatic factors varied with the season and the region. On the whole, the NDVI increased in three seasons, and the fluctuation in the NDVI in summer was consistent with that in the growth season, and the fluctuation in the NDVI in summer was consistent with that in the growth season, which was controlled mainly by precipitation, because summer contributes the most to annual productivity. The effect of temperature on the NDVI was marked in spring and autumn. Residual analysis showed that human activities has a major impact on changes in the NDVI, especially in areas with high population density (western alpine areas and central grassland areas of Mongolia), the decline in the NDVI is obviously caused by human activities.