Huang Yangbin, Lei Huimin, Duan Limin
Department of Hydraulic Engineering, Tsinghua University, Beijing 100084, China.
Department of Hydraulic Engineering, Tsinghua University, Beijing 100084, China.
Sci Total Environ. 2024 Nov 15;951:175495. doi: 10.1016/j.scitotenv.2024.175495. Epub 2024 Aug 16.
Drought and heatwave are the primary climate extremes for vegetation productivity loss in the global temperate semi-arid grassland, challenging the ecosystem productivity stability in these areas. Previous studies have indicated a significant decline in the resistance of global grassland productivity to drought, but we still lack a systematic understanding of the mechanisms determining the spatiotemporal variations in grassland resistance to drought and heatwave. In this study, we focused on temperate semi-arid grasslands of China (TSGC) to assess the spatiotemporal variations of grassland productivity resistance to different climate extremes: compound dry-hot events, individual drought events, and individual heatwave events that occurred during 2000-2019. Based on the explainable machine learning model, we explored the resistance to the interaction of drought and heatwave and identify the dominant factors determining the spatiotemporal variations in resistance. The results revealed that grassland resistance to climate extremes had decreased in Xilingol Grassland and Mu Us Sandy Land, and had a not significant increase in Otindag Desert during 2000-2019. Human activities and the increase in CO concentration causes a decline in resistance in Mu Us Sandy Land, and the increase of VPD and shift of vegetation loss event timing caused a decline in resistance in Xilingol Grassland, while the weakening of climate extremes, especially the shortening of drought duration, increase the resistance in Otindag Desert. Mean annual temperature dominates the spatial differences in resistance among different grasslands. When drought and heatwave occur simultaneously, there is an additive effect on resistance and causes lower resistance to compound dry-hot events compared to individual drought and heatwave events. Our analysis provides crucial insights into understanding the impact of climate extremes on the temperate semi-arid grasslands of China.
干旱和热浪是全球温带半干旱草原植被生产力损失的主要气候极端事件,对这些地区的生态系统生产力稳定性构成挑战。以往研究表明全球草地生产力对干旱的抗性显著下降,但我们仍缺乏对决定草地对干旱和热浪抗性时空变化机制的系统认识。在本研究中,我们聚焦于中国温带半干旱草原,评估2000 - 2019年期间草地生产力对不同气候极端事件(复合干热事件、单个干旱事件和单个热浪事件)抗性的时空变化。基于可解释机器学习模型,我们探究了对干旱和热浪相互作用的抗性,并确定了决定抗性时空变化的主导因素。结果表明,2000 - 2019年期间,锡林郭勒草原和毛乌素沙地的草地对气候极端事件的抗性下降,而浑善达克沙地的抗性无显著增加。人类活动和二氧化碳浓度增加导致毛乌素沙地的抗性下降,水汽压差增加和植被损失事件时间的变化导致锡林郭勒草原的抗性下降,而气候极端事件的减弱,尤其是干旱持续时间的缩短,增加了浑善达克沙地的抗性。年平均温度主导不同草地间抗性的空间差异。当干旱和热浪同时发生时,对抗性有累加效应,与单个干旱和热浪事件相比,对复合干热事件的抗性更低。我们的分析为理解气候极端事件对中国温带半干旱草原的影响提供了关键见解。