College of Horticulture and Plant Protection, Henan University of Science and Technology, Luoyang 471023, Henan Province, China.
State Key Laboratory of Severe Weather, Chinese Academy of Meteorological Sciences, Beijing 100081, China.
Sci Total Environ. 2024 Aug 15;938:173489. doi: 10.1016/j.scitotenv.2024.173489. Epub 2024 May 23.
Climate-induced changes in plant phenology and physiology are crucial in regulating terrestrial productivity and ecosystem functions. However, the spatiotemporal patterns of grassland phenology and its relationships with environmental factors remain unclear. We extracted phenological metrics from grasslands using the FLUXNET dataset (34 sites and 169 site-year). We then explored the spatiotemporal variations in phenological metrics, their relationships with gross primary productivity (GPP), and the driving mechanisms behind them using regression analysis and structural equation modeling methods. The start of the growing season (SOS) significantly advanced, whereas the end of the growing season (EOS) was slightly delayed (non-significant), leading to an extension of the growing season (LOS) (marginally significant) with increasing latitude northward. The multi-year averaged GPP in grassland sites was exponentially correlated with LOS and linearly correlated with maximum GPP (GPP). Phenological metrics exhibited linear relationships with mean annual temperature and quadratic relationships with mean annual precipitation (MAP). EOS, LOS, and GPP increased (SOS decreased) with MAP initially, then leveled off or decreased (SOS increased) when MAP reached a threshold of 1000 mm. Spatiotemporally, preseason soil water content (SWC) and air temperature significantly affected SOS, and wind speed was the dominant environmental driver for EOS. Structural equation modeling further suggested that decreasing wind speed might delay the EOS by reducing the atmospheric and soil dryness. In conclusion, our findings suggested that an improved grassland phenological model could project an advancing SOS, a delaying EOS, and an extension of LOS in response to decreasing wind speed and increased moisture in the future.
气候引起的植物物候和生理学变化对于调节陆地生产力和生态系统功能至关重要。然而,草原物候的时空格局及其与环境因素的关系仍不清楚。我们使用通量网数据集(34 个站点和 169 个站点年)提取了草原物候学指标。然后,我们使用回归分析和结构方程模型方法探讨了物候学指标的时空变化、它们与总初级生产力(GPP)的关系以及背后的驱动机制。生长季节开始(SOS)显著提前,而生长季节结束(EOS)略有延迟(不显著),导致生长季节延长(LOS)(略有显著),纬度向北增加。草原站点多年平均的 GPP 与 LOS 呈指数相关,与最大 GPP(GPP)呈线性相关。物候学指标与年平均温度呈线性关系,与年平均降水量(MAP)呈二次关系。EOS、LOS 和 GPP 随着 MAP 的增加而增加(SOS 减少),而当 MAP 达到 1000 mm 的阈值时,它们的增加(SOS 减少)逐渐趋于平稳或减少。在时空上, preseason土壤水分含量(SWC)和空气温度对 SOS 有显著影响,风速是 EOS 的主要环境驱动因素。结构方程模型进一步表明,风速的降低可能通过减少大气和土壤干燥度来延迟 EOS。总之,我们的研究结果表明,改进的草原物候模型可以预测 SOS 的提前、EOS 的延迟和 LOS 的延长,以应对未来风速的降低和湿度的增加。