1 | INTRODUCTIONThe ecosystem on the Tibetan Plateau is extremely fragile, and its ability to resist disturbance and regenerate is weak (Cui & Graf, 2009). The temperature of the Tibetan Plateau has been constantly increasing due to global warming, and the rate of warming on the plateau is higher than that in other parts of China (Cui & Graf, 2009; Piao et al., 2004). The study of the spatial and temporal distribution characteristics of vegetation and its climate response on the Tibetan Plateau is significant for deepening the understanding of trends in the ecological effects of climate change on vegetation degradation.The impact of climate change on vegetation occurs at different spatial and temporal scales, and it is difficult to meet the requirements for monitoring changes at regional or global scales with traditional monitoring methods (Pang et al., 2017). With its rapid development, remote sensing technology has realized the long-term monitoring of the dynamic changes in vegetation cover in certain regions, which has improved data availability for research on vegetation responses to climate (Potter & Brooks, 1998). In particular, widely available vegetation index data from the Moderate-Resolution Imaging Spectroradiometer (MODIS) and Advanced Very High Resolution Radiometer (AVHRR) are very useful for the successful assessment, detection, and depiction of landscape conditions and their responses to climate variations at both global and regional scales (Guo et al., 2014).Although NDVI data are strongly related to plant phenological variables and climatic parameters, these relationships are ecosystem-dependent, and can be highly site-specific (Prasad et al., 2008; Mingguo & Veroustraete, 2004) and vary widely in different ecosystems, such as soil ecosystems (FARRAR et al., 1994) and vegetation ecosystems (White et al., 1997). At present, most studies have examined the relationship between climate and vegetation at different scales, which reflects the spatial distribution of vegetation activity changes. Due to stratified heterogeneity, considering the property information (i.e., vegetation type, land cover type, etc.) of each pixel is very useful for understanding the mechanisms of the effect of climate on vegetation. Therefore, it is important to study the relationship between vegetation and climate factors at subregional scales. Among the many potential spatial scales for studies, it is most reasonable to explore climatic effects on different vegetation ecosystems (i.e., at the vegetation type scale). The response of different grassland systems to climate change can vary greatly (Li et al., 2018). The same type of vegetation will often have a similar climate environment and similar response mechanisms to climate factors.For a long time, temperature and water stress have been the primary considerations in studies on climate factors affecting vegetation activity (Wang et al., 2014). As research progresses, an increasing number of climate factors are being taken into account. Sunlight, i.e., solar radiation, provides an energy source for vegetative photosynthesis. On the Tibetan Plateau, sunshine has a more significant impact on vegetation in the southeast region of the plateau (Wang et al., 2014). The lack of radiation observation sites may be the main reason why the influence of radiation is rarely considered in studies, but the sunshine percentage may be a feasible replacement. The relative humidity can reflect the dry and wet conditions of an area to some extent and can have interactive effects with vegetation (Lin et al., 2013). Minimum temperature resistance can be a significant influencing factor on vegetation activity (Prasad et al., 2008; Woodward & McKee, 1991).The effect of precipitation on vegetation shows significant lag (Pang et al., 2017). Many studies have been carried out on the lag in the effect of precipitation on vegetation growth, indicating that the lag time of the climate factors that affect vegetation growth varies among different vegetation ecosystems and growth stages (Sivakumar, 1988; DAVENPORT & NICHOLSON, 1993; Capecchi et al., 2008; Philippon et al., 2005; Martiny et al., 2005). In addition to precipitation, some studies have been conducted on lag effects of other climate factors on vegetation. Piao. (2003) analyzed the monthly average NDVI variation and found that NDVI in April or May was significantly correlated with the temperature in February. Wen et al. (2017) analyzed the regional differences in the lag time of effects at the pixel scale, concluding that there was regional heterogeneity in the amount of lag in the effects of both precipitation and temperature. Revealing the lag in the effects of climate factors on vegetation is significant for understanding the ecological mechanisms of vegetation change.In this study, long-term GIMMS (Global Inventory Modeling and Mapping Studies) NDVI data and the precipitation, average temperature, average minimum temperature, average maximum temperature, relative humidity, sunshine percentage data from the same period were collected to study the spatial and temporal variation patterns of vegetation on the Tibetan Plateau and the ecological mechanisms of the response of vegetation to climate factors from 1985 to 2015. Based on the 1:1,000,000 vegetation type data for China, ten vegetation domain types and pure pixels for each type of vegetation were selected as the study area to reduce errors due to the coarse spatial resolution of NDVI. Because these climate factors affect vegetation activity in different ways and the relationships among them are also complex, stepwise regression was adopted, which can reduce the effects of collinearity between independent variables to some extent. Moreover, instead of simply using the meteorological data from the same period as the NDVI data, the regression equation for NDVI and meteorological data in the period when vegetation activity was the most strongly correlated with meteorological factors was calculated.