Abstract

In the Loess Plateau (LP) of China, the vegetation degradation and soil erosion problems have been shown to be curbed after the implementation of the Grain for Green program. In this study, the LP is divided into the northwestern semi-arid area and the southeastern semi-humid area using the 400 mm isohyet. The spatial–temporal evolution of the vegetation NDVI during 2000–2015 are analyzed, and the driving forces (including factors of climate, environment, and human activities) of the evolution are quantitatively identified using the geographical detector model (GDM). The results showed that the annual mean NDVI in the entire LP was 0.529, and it decreased from the semi-humid area (0.619) to the semi-arid area (0.346). The mean value of the coefficient of variation of the NDVI was 0.1406, and it increased from the semi-humid area (0.1165) to the semi-arid area (0.1926). The annual NDVI growth rate in the entire LP was 0.0079, with the NDVI growing faster in the semi-humid area (0.0093) than in the semi-arid area (0.0049). The largest increments of the NDVI were from grassland, farmland, and woodland. The GDM results revealed that changes in the spatial distribution of the NDVI could be primarily explained by the climatic and environmental factors in the semi-arid area, such as precipitation, soil type, and vegetation type, while the changes were mainly explained by the anthropogenic factors in the semi-humid area, such as the GDP density, land-use type, and population density. The interactive analysis showed that interactions between factors strengthened the impacts on the vegetation change compared with an individual factor. Furthermore, the ranges/types of factors suitable for vegetation growth were determined. The conclusions of this study have important implications for the formulation and implementation of ecological conservation and restoration strategies in different regions of the LP.

Highlights

  • Vegetation plays an indispensable role in regional terrestrial ecosystems, and constitutes an essential link between soil, water, and atmosphere

  • Vegetation coverage effectively reduces the surface soil erosion caused by exogenous forces such as wind, diminishes the splash erosion caused by raindrops, alleviates the hydrodynamic erosion of rivers, and improves the soil environment

  • It is of crucial importance to explore the vegetation coverage changes and dynamics for the soil erosion prevention and control, ecological environmental protection, and sustainable social and economic development [3,4]

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Summary

Introduction

Vegetation plays an indispensable role in regional terrestrial ecosystems, and constitutes an essential link between soil, water, and atmosphere. Vegetation coverage effectively reduces the surface soil erosion caused by exogenous forces such as wind, diminishes the splash erosion caused by raindrops, alleviates the hydrodynamic erosion of rivers, and improves the soil environment. The main monitoring method used in large-scale vegetation coverage change research is based on satellite remote sensing because of its wide spatial range and gradually improving resolution, which effectively makes up for the shortcomings of traditional monitoring methods [5]. The NDVI can be used to quantitatively evaluate the regional vegetation coverage and growth, which is considered to be an effective indicator for monitoring terrestrial vegetation changes, and has been widely used in research and management in various fields, such as agriculture and ecology [8]

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