Abstract

Research on vegetation variation is an important aspect of global warming studies. The quantification of the relationship between vegetation change and climate change has become a central topic and challenge in current global change studies. The source region of the Yellow River (SRYR) is an appropriate area to study global change because of its unique natural conditions and vulnerable terrestrial ecosystem. Therefore, we chose the SRYR for a case study to determine the driving forces behind vegetation variation under global warming. Using the Normalized Difference Vegetation Index (NDVI) and climate data, we investigated the NDVI variation in the growing season in the region from 1998 to 2016 and its response to climate change based on trend analysis, the Mann–Kendall trend test and partial correlation analysis. Finally, an NDVI–climate mathematical model was built to predict the NDVI trends from 2020 to 2038. The results indicated the following: (1) over the past 19 years, the NDVI showed an increasing trend, with a growth rate of 0.00204/a. There was an upward trend in NDVI over 71.40% of the region. (2) Both the precipitation and temperature in the growing season showed upward trends over the last 19 years. NDVI was positively correlated with precipitation and temperature. The areas with significant relationships with precipitation covered 31.01% of the region, while those with significant relationships with temperature covered 56.40%. The sensitivity of the NDVI to temperature was higher than that to precipitation. Over half (56.58%) of the areas were found to exhibit negative impacts of human activities on the NDVI. (3) According to the simulation, the NDVI will increase slightly over the next 19 years, with a linear tendency of 0.00096/a. From the perspective of spatiotemporal changes, we combined the past and future variations in vegetation, which could adequately reflect the long-term vegetation trends. The results provide a theoretical basis and reference for the sustainable development of the natural environment and a response to vegetation change under the background of climate change in the study area.

Highlights

  • Global environmental change, which is marked by “global warming”, has possible serious impacts on ecosystems and has attracted great attention from scientists around the world [1,2]

  • The results showed that the Normalized Difference Vegetation Index (NDVI) exhibited a slowly increasing trend with obvious regional characteristics

  • This study provides a scientific basis for the development of countermeasures to protect vegetation in the source region of the Yellow River (SRYR) under the background of global warming

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Summary

Introduction

Global environmental change, which is marked by “global warming”, has possible serious impacts on ecosystems and has attracted great attention from scientists around the world [1,2]. As the main component of terrestrial ecosystems, vegetation is a sensitive indicator of climate change. The NDVI is widely used in global and regional vegetation change research. Relevant research has shown that the vegetation in China has exhibited the same trend. The results showed that the NDVI exhibited a slowly increasing trend with obvious regional characteristics. Piao and Fang used global inventory modeling and mapping studies (GIMMS) NDVI data to analyse the vegetation cover in China from 1982 to 1999, and showed that 86.2% of China’s area exhibited an increasing trend in vegetation. Other scholars have performed extensive research on vegetation cover changes in the Huang-Huai-Hai River basin [11], in the Yangtze River basin [12], on the Qinghai–Tibet Plateau [13], and in the southwestern karst region [14]. The Qinghai–Tibet Plateau was shown to be more sensitive to the effects of climate warming than other regions

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