Abstract

Vegetation regulates the exchange of terrestrial carbon and water fluxes and connects the biosphere, hydrosphere, and atmosphere. Over the last four decades, vegetation greening has been observed worldwide using satellite technology. China has also experienced a notably widespread greening trend. However, the responsiveness of vegetation dynamics to elevated CO2 concentration, climate change, and human activities remains unclear. In this study, we attempted to explore the impact of natural (precipitation, air temperature), biogeochemical (CO2), and anthropogenic drivers (nighttime light, afforestation area) on changes in vegetation greenness in the Haihe River Basin (HRB) during 2002–2018 at the county-level. We further determined the major factors affecting the variation in satellite-derived normalized difference vegetation index (NDVI) from moderate resolution imaging spectroradiometer (MODIS) for each county. The results indicated that over 85% of the counties had a significantly increased NDVI trend, and the average linear trend of annual NDVI across the study region was 0.0037 per year. The largest contributor to the NDVI trend was CO2 (mean contribution 45%), followed by human activities (mean contribution of 27%). Additionally, afforestation was a pronounced driving force for NDVI changes in mountainous areas, resulting from ecosystem restoration efforts. Our findings emphasize the crucial role of CO2 fertilization in vegetation cover change, while considering CO2 concentration, climate change, and human activities, and shed light on the significant influences of afforestation programs on water resources, especially in mountainous areas.

Highlights

  • The study area was reclassified as mixed grassland (MG), mixed cropland (MC), mixed forestland (MF), along with other types

  • We especially focused on the influence of CO2 and afforestation on normalized difference vegetation index (NDVI), which has not been done in the Haihe River Basin (HRB) before

  • We quantified the impact of natural, biogeochemical, and anthropogenic drivers on greenness trends indicated by the NDVI in the HRB region, determined the major factors influencing the variations in NDVIs for each county, and predicted the future NDVI for the 21st century

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Summary

Introduction

Publisher’s Note: MDPI stays neutral with regard to jurisdictional claims in published maps and institutional affiliations. Vegetation controls the exchange of terrestrial carbon and water cycles between the ground surface and the atmosphere through photosynthesis. It alters the momentum and energy absorption via its physiological properties [1,2]. Carbon uptake by vegetation is a major CO2 sink on the land. Because vegetation greening and browning are associated with variations in carbon storage, water availability, surface energy, soil nutrients, terrestrial hydrometeorology, and eco-hydrological processes, quantifying the reason for vegetation change has attracted considerable attention from scientists and policymakers [3,4,5,6]

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