Abstract
Temporal and spatial changes in vegetation and their influencing factors are of great significance for the assessment of climate change and sustainable development of ecosystems. This study applied the Asymmetric Gaussians (AG) fitting method, Mann-Kendall test, and correlation analysis to the Global Inventory Monitoring and Modeling System (GIMMS) third-generation Normalized Difference Vegetation Index and gridded climate and drought data for 1982–2015. The temporal and spatial changes to NDVI for natural grassland and forest during the growing season were analyzed. Relationships among NDVI, climate change, and droughts were also analyzed to reveal the influence of vegetation change. The results showed that: (1) Land use/cover change (LUCC) in China was mainly represented by increases in agricultural land (Agrl) and urban and rural land (Uril), and decreases in unutilized land (Bald), grassland, forest, and permanent glacier and snow (Snga). The increase in agricultural land was mainly distributed in the western northwest arid area (WNW) and northern North China (NNC), whereas regions with severe human activities such as southern South China (SNC), western South China (WSC), and eastern South China (ESC) showed significant decreases in agricultural land due to conversion to urban and rural land. (2) The start of the growing season (SOS) was advanced in WNW, SNC, WSC, and ESC, and the end of growing season (EOS) was delayed in WNW, NNC, and SNC. The growing season length (GSL) of natural vegetation in China has been extended by eight days over the last 34 years. However, the phenology of the Qinghai-Tibet Plateau (TP) was opposite to that of the other regions and the GSL showed an insignificant decreasing trend. (3) The NDVI increased significantly, particularly in the SNC, WSC, ESC, and the grassland of the WNW. Precipitation was found to mainly control the growth of vegetation in the arid and semi-arid regions of northwest China (WNW and ENW), and precipitation had a much greater impact on grassland than on forests. Temperature had an impact on the growth of vegetation throughout China, particularly in SNC, ESC, and WSC. (4) The Standardized Precipitation Evapotranspiration Index (SPEI) showed a downward trend, indicating an aridification trend in China, particularly in ENW, NNC, and WNW. Similar to precipitation, the main areas affected by drought were WNW and ENW and grassland was found to be more sensitive to drought than forest. The results of this study are of great significance for predicting the response of ecosystem productivity to climate change under future climate change scenarios.
Highlights
As an important component of the terrestrial ecosystem, vegetation is a natural link connecting soil, atmosphere, and water
Since the current study focused on the effects of drought on vegetation during the growing season, the Standardized Precipitation Evapotranspiration Index (SPEI) data at a 6-month time scale (SPEI6) was used for analysis
Agricultural land (Agrl) and water increased by 33% and 20% in western northwest arid area (WNW), respectively, mainly due to the conversion of unutilized land (Bald) and grassland
Summary
As an important component of the terrestrial ecosystem, vegetation is a natural link connecting soil, atmosphere, and water. Vegetation plays a pivotal role in the ecosystem and can act as an “indicator” within the study of global change. The growth status of vegetation is closely related to environmental factors, such as climate, water quality, and topography [1]. Climate change has altered the growth environment of plants, thereby affecting the growth of vegetation. Global changes have had a significant impact on the structure and function of terrestrial ecosystems [2,3,4]. Understanding the inherent relationship between vegetation and climate can illuminate the role of climate in changes to the terrestrial ecosystem
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