Huiqing Lin

and 5 more

As an essential pathway for nature-based solutions, vegetation restoration can effectively absorb carbon sequestration and mitigate global warming. However, the excessive water consumption by vegetation expansion may create potential water conflicts between natural ecosystems and human systems, and even exacerbate local water shortages, especially in water-limited dryland regions. By evaluating water availability using multiple datasets, this study explored the vegetation restoration potential and the allowable vegetation conversion in China’s drylands under the constraint of water availability. We found that the additional water resources available for vegetation restoration in China’s drylands were 2.7 ± 11 mm (median ± SD) from 2003 to 2018 but it decreased over the period (-1.15 mm yr-1). 45.0% of the drylands area had water deficits, after considering existing vegetation and human water consumption. Under current water constraints, additional gross primary productivity (GPP) that could be restored ranged from 4% to 7% depending on vegetation types (7.1% for forests, 6.1% for grasslands, 4.3% for irrigated crops, and 5.6% for rain-fed crops). In water surplus areas, primarily in the south and east of China’s drylands, most vegetation conversions toward higher-water-consumption types were allowed to occur. In water deficit areas, the west of drylands, even converting all the existing vegetation to less water-intensive types would not compensate for the water deficit in most regions, suggesting local vegetation may have exceeded the water-carrying capacity. Our research highlights the importance of the potential water constraint of vegetation restoration in drylands and provides guidance for decision-making vegetation restoration while ensuring water sustainability.

Huiqing Lin

and 2 more

Bowen ratio reflects the partitioning between sensible and latent heat fluxes and plays a crucial role in land-atmosphere interaction. In this study, the spatiotemporal variations of Bowen ratio among 12 vegetation types were analyzed using observations from 203 FLUXNET sites worldwide and compared against Community Land Model. Results showed that the annual mean Bowen ratio across all sites was 1.48 ± 1.20 (mean ± SD). Sites with Bowen ratios less than 1 (39%, 80 sites) were found across all continents, and the ones with higher Bowen ratios (>3)(7%, 14 sites) appeared in dry and warm areas. Open shrublands showed the highest Bowen ratio (3.04 ± 0.58), whereas wetlands showed the lowest (0.74 ± 0.09). In terms of seasonality, Bowen ratio showed a U-curve with lower values in local summer and higher in spring and autumn in the northern hemisphere; the opposite occurred in the southern hemisphere. The spatiotemporal variations in Bowen ratio can be explained by climatic, geographical, and biological factors, with climate factors having the greatest impact. Bowen ratio increased under higher VPD (R = 0.45) and hotter (R=0.14) conditions with more shortwave radiation (R=0.39), and decreased with higher precipitation (R=-0.34), albedo (R=-0.16), and leaf area index (R=-0.25). CLM well reproduced the global annual mean Bowen ratio, but showed larger differences for certain vegetations types such as open shrublands (-1.51), woody savannas (+0.98). Our results could enhance our understanding of biotic and environmental controls on land surface energy fluxes and help improve land surface and climate models.