State Key Laboratory of Vegetation and Environmental Change, Institute of Botany, Chinese Academy of Sciences, Beijing, China.
University of Chinese Academy of Sciences, Beijing, China.
Glob Chang Biol. 2020 May;26(5):3015-3027. doi: 10.1111/gcb.15051. Epub 2020 Mar 25.
Global warming has greatly altered winter snowfall patterns, and there is a trend towards increasing winter snow in semi-arid regions in China. Winter snowfall is an important source of water during early spring in these water-limited ecosystems, and it can also affect nutrient supply. However, we know little about how changes in winter snowfall will affect ecosystem productivity and plant community structure during the growing season. Here, we conducted a 5-year winter snow manipulation experiment in a temperate grassland in Inner Mongolia. We measured ecosystem carbon flux from 2014 to 2018 and plant biomass and species composition from 2015 to 2018. We found that soil moisture increased under deepened winter snow in early growing season, particularly in deeper soil layers. Deepened snow increased the net ecosystem exchange of CO (NEE) and reduced intra- and inter-annual variation in NEE. Deepened snow did not affect aboveground plant biomass (AGB) but significantly increased root biomass. This suggested that the enhanced NEE was allocated to the belowground, which improved water acquisition and thus contributed to greater stability in NEE in deep-snow plots. Interestingly, the AGB of grasses in the control plots declined over time, resulting in a shift towards a forb-dominated system. Similar declines in grass AGB were also observed at three other locations in the region over the same time frame and are attributed to 4 years of below-average precipitation during the growing season. By contrast, grass AGB was stabilized under deepened winter snow and plant community composition remained unchanged. Hence, our study demonstrates that increased winter snowfall may stabilize arid grassland systems by reducing resource competition, promoting coexistence between plant functional groups, which ultimately mitigates the impacts of chronic drought during the growing season.
全球变暖极大地改变了冬季降雪模式,中国半干旱地区冬季降雪有增加的趋势。冬季降雪是这些水资源有限的生态系统早春的重要水源,也会影响养分供应。然而,我们对冬季降雪变化如何影响生长季生态系统生产力和植物群落结构知之甚少。在这里,我们在内蒙温带草原进行了为期 5 年的冬季积雪处理实验。我们测量了 2014 年至 2018 年的生态系统碳通量,以及 2015 年至 2018 年的植物生物量和物种组成。我们发现,在早春,深层冬季积雪会增加土壤水分,特别是在较深的土壤层。积雪加深增加了净生态系统交换的 CO(NEE),并减少了 NEE 的年内和年际变化。积雪加深对地上植物生物量(AGB)没有影响,但显著增加了根生物量。这表明增强的 NEE被分配到地下,这提高了水分获取能力,从而有助于在深雪斑块中 NEE 更稳定。有趣的是,对照小区的草 AGB 随时间下降,导致以草本植物为主的系统向以草本植物为主的系统转变。在同一时间框架内,该地区的另外三个地点也观察到草 AGB 的类似下降,这归因于生长季 4 年的平均降水量低于平均值。相比之下,在积雪加深的情况下,草 AGB 得到了稳定,植物群落组成保持不变。因此,我们的研究表明,增加冬季降雪可能通过减少资源竞争来稳定干旱草原系统,促进植物功能群的共存,从而减轻生长季慢性干旱的影响。