Effects of Effective Precipitation and Accumulated Temperature on the Terrestrial EVI (Enhanced Vegetation Index) in the Yellow River Basin, China

• Published in: Atmosphere Vol. 13; no. 10; p. 1555
• Main Authors: Wang, Huiliang, He, Linpo, Yin, Jun, Yu, Zhilei, Liu, Simin, Yan, Denghua
• Format: Journal Article
• Language: English
• Published: Basel MDPI AG 01.10.2022
• Subjects: accumulated temperature (At); Agricultural land; Aquatic ecosystems; Atmospheric temperature; Climate and vegetation; Climate change; Conservation; Correlation analysis; Ecosystems; Effective precipitation; effective precipitation (Epr); enhanced vegetation index (EVI); Environmental aspects; Forest ecosystems; Grasslands; hydrothermal condition; Meteorological data; MODIS; Precipitation; Precipitation (Meteorology); rainfall; Regional climates; Regression analysis; River basins; River ecology; Rivers; Sustainable development; Temperature; Temperature effects; Temporal variations; Terrestrial ecosystems; Trends; Vegetation; Vegetation dynamics; Vegetation index; Wetlands; Yellow River basin (YRB); China; Loess Plateau; Yellow River
• ISSN: 2073-4433; 2073-4433
• DOI: 10.3390/atmos13101555

To identify the vegetation dynamics and relationship with the hydrothermal conditions in the Yellow River basin (YRB), the spatial–temporal variations of EVI, effective precipitation (Epr), accumulated temperature (At), and their relationships were obtained based on the MODIS EVI data and meteorological data from the YRB during 2001–2020. The results indicate that EVI trends increased during 2001 to 2020, especially in the farmland, forestland, and grassland ecosystems. Epr and At have also increased over the last 20 years. Epr mostly increased faster in the grassland, and water bodies and wetland ecosystems. At mostly increased faster in the water bodies and wetland, desert, and forest ecosystems. Affected by Epr and At, the correlation between the EVI and hydrothermal conditions varied under different hydrothermal conditions. Compared to the At, the Epr was the restrictive factor for the EVI variations in the terrestrial ecosystem in the YRB. In addition, the dynamical thresholds of the EVI, Epr, and At were confirmed. This study can improve the understanding of vegetation variations and their response to regional climate change, which is critical for ecological conservation and the high-quality development of the YRB.