Abstract

Alpine vegetation on the Tibetan Plateau (TP) is known to be sensitive to both climate change and anthropogenic disturbance. However, the magnitude and patterns of alpine vegetation dynamics and the driving mechanisms behind their variation on the TP remains under debate. In this study, we used updated MODIS Collection 6 Normalized Difference Vegetation Index (NDVI) from the Terra satellite combined with linear regression and the Break for Additive Season and Trend model to reanalyze the spatiotemporal patterns of vegetation change on the TP during 2000–2015. We then quantified the responses of vegetation variation to climatic and anthropogenic factors by coupling climatic and human footprint datasets. Results show that growing season NDVI (GNDVI) values increased significantly overall (0.0011 year−1, p < 0.01) during 2000–2015 and that 70.37% of vegetated area on the TP (23.47% significantly with p < 0.05) exhibited greening trends with the exception of the southwest TP. However, vegetation greenness experienced trend shifts from greening to browning in half of the ecosystem zones occurred around 2010, likely induced by spatially heterogeneous temporal trends of climate variables. The vegetation changes in the northeastern and southwestern TP were water limited, the mid-eastern TP exhibited strong temperature responses, and the south of TP was driven by a combination of temperature and solar radiation. Furthermore, we found that, to some extent, anthropogenic disturbances offset climate-driven vegetation greening and aggravated vegetation browning induced by water deficit. These findings suggest that the impact of anthropogenic activities on vegetation change might not overwhelm that of climate change at the region scale.

Highlights

  • Climate-induced changes in vegetation can feedback into the climate-vegetation-soil continuum via various biotic and abiotic interactions [1,2]

  • In this study, based on the updated Normalized Difference Vegetation Index (NDVI) form MODerate resolution Imaging Spectroradiometer (MODIS) Terra-Collection 6 (C6), we found that 70.37% of vegetated areas of the Tibetan Plateau (TP) (23.47% significantly with p < 0.05) exhibited greening trends and the change percentages of growing season NDVI (GNDVI) were positive across all elevation bins and most ecosystem zones over the TP during the past 16 years (Figures 2 and 3)

  • We revisited the spatiotemporal patterns of vegetation change and its major underlying drivers on the TP during 2000–2015 based on the updated NDVI form MODIS Terra-C6

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Summary

Introduction

Climate-induced changes in vegetation can feedback into the climate-vegetation-soil continuum via various biotic and abiotic interactions [1,2]. The spatiotemporal variability in vegetation growth can be attributed to the heterogeneity of either climate change or anthropogenic influences, or of both [1,3,4,5]. Monitoring and attributing such spatiotemporal changes in vegetation growth is critical to understanding the role that this land cover type plays in the Earth’s climatic system [6], but is a requirement for developing more sustainable strategies and policies for ecosystem management [7,8]. A range of evaluation studies have, noted the fact that these remote sensing products did not yield consistent patterns of vegetation change [12,13,14,15], likely due to the impacts of sensor shifts or degradation [14,16,17]. The widespread areas of browning identified by MODIS Collection 5 (C5) vegetation indices from the Terra satellite could not be detected by Collection 6 (C6) vegetation indices, which is mainly because the algorithm used in the former did not take the effects of sensor degradation into account [14,16]

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