UNI-MB - logo
UMNIK - logo
 
E-resources
Full text
Peer reviewed
  • Soil moisture alters the re...
    Zhang, Tao; Shan, Baoxin; Xu, Mingjie; Zhao, Guang; Zheng, Zhoutao; Tang, Yuanyuan; Chen, Ning; Zhu, Juntao; Cong, Nan; Niu, Ben; Zhang, Yangjian

    The Science of the total environment, 10/2024, Volume: 947
    Journal Article

    Water availability, which can be represented by soil water content (SWC), plays a crucial role in plant growth and productivity across the cold and arid Qinghai-Tibetan Plateau. However, the indirect effects of SWC are less well understood, and a more comprehensive understanding of its regulating effects may enhance the recognition of its importance, as this factor is pivotal for accurately predicting the future response of alpine ecosystems to climate change. In this study, in situ eddy covariance observation data from typical alpine ecosystems and satellite data covering the Qinghai-Tibetan region were used to comprehensively reveal the effects of SWC on ecosystem productivity. The results indicated that SWC played an important role in regulating the responses of gross primary productivity (GPP) to other environmental factors over both time and space, especially in terms of the responses of GPP to vapor pressure deficit (VPD). The regulating effect can be summarized as follows: there was a specific SWC value (SWC = 0.24 m3 m−3 on the Qinghai-Tibetan Plateau) above which SWC was no longer the primary limiting factor. The responses of GPP to certain environmental factors shifted from negative to positive when the SWC increased above this value. The responses of GPP to VPD exhibited the highest sensitivity to the regulating effects of SWC, with a general response pattern found across different temporal and spatial scales. The findings revealed divergent responses of GPP to environmental factors under different SWC conditions and between arid and humid regions, emphasizing the importance of soil water conditions. These findings suggest that water conditions should be given primary consideration in global change studies. Display omitted •The soil water content (SWC) controlled the alpine ecosystem productivity (GPP).•The responses of GPP to other factors shifted by an SWC threshold of 0.24 m3 m−3.•SWC threshold (0.24) was verified and applicable at multiple spatiotemporal scales.•From arid to humid, the VPD shifted from a negative factor to a positive factor.•SWC would determine the responses of alpine ecosystems to future climate change.