Vegetation change (VC) plays a crucial role in driving fluctuations in ecosystem biomass. However, VC encompasses either natural growth (NG) or artificial restoration (AR), and the specific effects of these two processes on biomass remain inadequately understood. The present study employed an ecohydrological model to evaluate the impacts of NG and AR on biomass in the Chinese Yellow River Basin (YRB) from 1998 to 2020. The results indicate that, over the past 23 years, NG led to 10.3 g C m−2 (8.4 %) increase in biomass, while AR resulted in somewhat less increase in biomass with just 6.6 g C m−2 (5.0 %). Overall, VC contributed to a 13.7 % increase in biomass. In most (84.8 %) regions within the YRB, VC positively contributed to biomass enhancement. The biomass increases attributed to NG mainly occur in the northern and northwestern YRB, encompassing 46.3 % of the total basin area. In contrast, regions where AR dominated biomass accumulation are spatially opposite to those primarily influenced by NG, with mostly being located in the southeastern and western YRB. The biomass responses to VC, NG, and AR exhibited pronounced differences across different ecosystem types. Farmlands experienced the most substantial biomass enhancement, followed by forest and grassland ecosystems, while desert ecosystem was the least affected. These findings suggested that, for the whole YRB, NG is more effective than AR in carbon sequestration. This is especially true for the northern and northwestern YRB where climate is more arid. However, in the southeastern YRB and the margianl area of Tibetan Plateau, AR is fine for the ecosystem health and biomass restoration in the region.
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