Spatiotemporal Variation of Vegetation on the Qinghai–Tibet Plateau and the Influence of Climatic Factors and Human Activities on Vegetation Trend (2000–2019)

Junhan Chen,Qi Lu,Feng Yan

doi:10.3390/rs12193150

Abstract

Vegetation is the terrestrial ecosystem component most sensitive to climate change. The Qinghai–Tibet Plateau (QTP), characterized by a cold climate and vulnerable ecosystems, has experienced significant warming in previous decades. Identifying the variation in vegetation coverage and elucidating its main driving factors are critical for ecological protection on the QTP. In this study, MOD13A2 Normalized Difference Vegetation Index (NDVI) data in the growing season (May to September) was used to represent QTP vegetation coverage during 2000–2019. The univariate linear regression, partial correlation analysis, residual analysis, and the Hurst exponent were used to detect the vegetation spatiotemporal dynamic, analyze the relationship between the vegetation and main driving factors, and predict the future vegetation dynamic. The growing season NDVI (GNDVI) of the QTP showed an extremely significant rate of increase (0.0011/a) during the study period, and 79.29% of the vegetated areas showed a greening trend. Over the past 20 years, the northeast, mid-east, and western edges of the plateau have been cooling and wetting, while the southwest, mid-west, and southeast have been warming and drying. Different climatic conditions lead to spatial differences in the response of plateau vegetation to climatic factors with generally 1–4 months lag time. The vegetation in the north of the plateau was mainly positively correlated with moisture, and negatively correlated with temperature, while the southern part showed positive correlation with temperature and negative correlation with moisture. Due to the enhancement of cooling and wetting trend in the last decade (2010–2019), especially in the south of the plateau, the greening trend of the plateau vegetation slowed down appreciably and even degraded in some areas. Human activities were mainly concentrated in the eastern part of the plateau—and its positive effect on vegetation was gradually increasing in most areas during study period, especially in the northeastern part. However, vegetation degradation caused by human activities in the southeast of the plateau should not be ignored. The future vegetation dynamic based on the Hurst exponent showed that the plateau faces a higher risk of vegetation degradation, which deserves more attention. This study explored the effect of climatic factors and human activities on vegetation of the QTP, thereby providing some guidance for the study of vegetation dynamic in the alpine areas.

Highlights

The world has experienced significant warming over the past few decades, and this warming has produced a significant impact on vegetation [1,2,3]
We studied the lag response between the growing season NDVI (GNDVI) and climatic factors at an interval of eight days, and took the date corresponding to the maximum partial correlation coefficient as the hysteresis time
Because of the spatially heterogeneous of climatic conditions, the response of vegetation on the plateau to climatic factors has formed obvious spatial differences: The northeast and southwest vegetation was negatively correlated with temperature and positively correlated with moisture

Summary

Introduction

The world has experienced significant warming over the past few decades, and this warming has produced a significant impact on vegetation [1,2,3]. The Qinghai–Tibet Plateau (QTP), located in southwestern China, is the largest geographical entity with the highest elevation. It is commonly called the “Third Pole” because the mean annual temperature of most areas of the QTP is

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