Institute of Soil and Water Conservation, Northwest A&F University, Yangling, Shaanxi 712100, PR China.
State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Northwest A&F University, Yangling, Shaanxi 712100, PR China.
Sci Total Environ. 2022 Jun 25;827:154351. doi: 10.1016/j.scitotenv.2022.154351. Epub 2022 Mar 5.
Increased atmospheric greenhouse gas (GHG) concentrations resulting from human activities lead to climate change, including global warming and changes of precipitation patterns worldwide, which in turn would have profound effects on soil GHG emissions. Nonetheless, the impact of the combination of warming and precipitation changes on all three major biogenic GHGs (CO, CH and NO) has not been synthesized, to build a global synthesis. In this study, we conducted a global meta-analysis concerning the effects of warming and precipitation changes and their interactions on soil GHG fluxes and explored the potential factors by synthesizing 39 published studies worldwide. Across all studies, combination of warming and increased precipitation showed more significant effect on CO emissions (24.0%) than the individual effect of warming (8.6%) and increased precipitation (20.8%). Additionally, warming increased NO emissions (28.3%), and decreased precipitation reduced CO (-8.5%) and NO (-7.1%) emissions, while the combination of warming and decreased precipitation also showed negative effects on CO (-7.6%) and NO (-14.6%) emissions. The interactive effects of warming and precipitation changes on CO emissions were usually additive, whereas CO and NO emissions were dominated by synergistic effects under warming and decreased precipitation. Moreover, climate, biome, duration, and season of manipulations also affected soil GHG fluxes as well. Furthermore, we also found the threshold effects of changes in soil temperature and moisture on CO and NO emissions under warming and precipitation changes. The findings indicate that both warming and precipitation changes substantially affect GHG emissions and highlight the urgent need to study the effect of the combination of warming and precipitation changes on C and N cycling under ongoing climate change.
人类活动导致大气温室气体(GHG)浓度增加,从而导致气候变化,包括全球变暖以及全球降水模式的变化,这反过来又会对土壤 GHG 排放产生深远影响。尽管如此,变暖与降水变化的组合对所有三种主要生物成因 GHG(CO、CH 和 NO)的影响尚未综合起来,以建立全球综合研究。在这项研究中,我们进行了一项全球荟萃分析,研究了变暖和降水变化及其相互作用对土壤 GHG 通量的影响,并通过综合全球 39 项已发表的研究来探索潜在因素。在所有研究中,变暖与增加降水的组合对 CO 排放的影响(24.0%)大于单独变暖(8.6%)和增加降水(20.8%)的影响。此外,变暖增加了 NO 排放(28.3%),减少降水减少了 CO(-8.5%)和 NO(-7.1%)排放,而变暖与减少降水的组合对 CO(-7.6%)和 NO(-14.6%)排放也有负面影响。变暖和降水变化对 CO 排放的相互作用通常是相加的,而在变暖和减少降水的情况下,CO 和 NO 排放则主要受到协同作用的影响。此外,气候、生物群落、处理持续时间和季节也会影响土壤 GHG 通量。此外,我们还发现了在变暖与降水变化下,土壤温度和水分变化对 CO 和 NO 排放的阈值效应。研究结果表明,变暖和降水变化都会对 GHG 排放产生重大影响,并强调了在当前气候变化下迫切需要研究变暖与降水变化对 C 和 N 循环的综合影响。