To fully understand the effects of climate change on grassland, interannual variation of vegetation coverage and its responses to meteorological variables in Naqu Prefecture of northern Tibet were investigated. This was done based on a Normalized Difference Vegetation Index (NDVI) dataset and historical meteorological data from 2000 to 2009. The NDVI dataset was downloaded from an Earth Observing System (EOS) data center. The meteorological data were retrieved from six meteorological stations of the China Meteorological Administration. Results show that NDVI had a significant increasing trend in the east, but no clear trend in the west. The NDVI in alpine meadows and alpine meadow steppes increased during the observation period. There were significant positive linear correlations between NDVI and water/heat conditions, and correlation between monthly mean minimum temperature (AMIT) and NDVI was the strongest. The strongest correlation between NDVI and heat conditions appeared at alpine meadows. Mean monthly wind velocity (MMWV) was negatively correlated with NDVI (p < 0.001), and the highest correlation was for alpine meadow steppes. There was a lag response of NDVI to water/heat conditions. The lag time of NDVI to precipitation and temperature was one month, but that to accumulated precipitation was two months.
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