Department of Biological Sciences, University of Illinois at Chicago, Chicago, IL, 60607, USA.
Department of Biological Sciences, University of Alaska, Anchorage, Anchorage, AK, 99501, USA.
Glob Chang Biol. 2016 Aug;22(8):2818-33. doi: 10.1111/gcb.13242. Epub 2016 May 9.
Arctic winter precipitation is projected to increase with global warming, but some areas will experience decreases in snow accumulation. Although Arctic CH4 emissions may represent a significant climate forcing feedback, long-term impacts of changes in snow accumulation on CH4 fluxes remain uncertain. We measured ecosystem CH4 fluxes and soil CH4 and CO2 concentrations and (13) C composition to investigate the metabolic pathways and transport mechanisms driving moist acidic tundra CH4 flux over the growing season (Jun-Aug) after 18 years of experimental snow depth increases and decreases. Deeper snow increased soil wetness and warming, reducing soil %O2 levels and increasing thaw depth. Soil moisture, through changes in soil %O2 saturation, determined predominance of methanotrophy or methanogenesis, with soil temperature regulating the ecosystem CH4 sink or source strength. Reduced snow (RS) increased the fraction of oxidized CH4 (Fox) by 75-120% compared to Ambient, switching the system from a small source to a net CH4 sink (21 ± 2 and -31 ± 1 mg CH4 m(-2) season(-1) at Ambient and RS). Deeper snow reduced Fox by 35-40% and 90-100% in medium- (MS) and high- (HS) snow additions relative to Ambient, contributing to increasing the CH4 source strength of moist acidic tundra (464 ± 15 and 3561 ± 97 mg CH4 m(-2) season(-1) at MS and HS). Decreases in Fox with deeper snow were partly due to increases in plant-mediated CH4 transport associated with the expansion of tall graminoids. Deeper snow enhanced CH4 production within newly thawed soils, responding mainly to soil warming rather than to increases in acetate fermentation expected from thaw-induced increases in SOC availability. Our results suggest that increased winter precipitation will increase the CH4 source strength of Arctic tundra, but the resulting positive feedback on climate change will depend on the balance between areas with more or less snow accumulation than they are currently facing.
随着全球变暖,北极冬季降水预计会增加,但某些地区的积雪量将会减少。尽管北极 CH4 排放可能代表着重要的气候强迫反馈,但积雪量变化对 CH4 通量的长期影响仍不确定。我们测量了生态系统 CH4 通量以及土壤 CH4 和 CO2 浓度和(13)C 组成,以研究经过 18 年的实验性雪深增加和减少后,在生长季节(6 月至 8 月)期间,驱动湿润酸性冻原 CH4 通量的代谢途径和传输机制。较深的积雪增加了土壤湿度和升温,降低了土壤中 O2 的水平,并增加了解冻深度。土壤湿度通过改变土壤 O2 饱和度来决定甲烷营养菌或产甲烷菌的优势,而土壤温度则调节着生态系统 CH4 汇或源的强度。与对照相比,减少的积雪(RS)增加了氧化 CH4(Fox)的分数,增加了 75-120%,使系统从一个小的源转变为一个净 CH4 汇(对照和 RS 分别为 21±2 和-31±1 mg CH4 m(-2) season(-1))。与对照相比,中等(MS)和高(HS)雪量增加分别使 Fox 减少了 35-40%和 90-100%,这有助于增加湿润酸性冻原的 CH4 源强度(MS 和 HS 分别为 464±15 和 3561±97 mg CH4 m(-2) season(-1))。Fox 随积雪深度的减少部分归因于与高大禾草扩张相关的植物介导的 CH4 传输增加。较深的积雪增加了新解冻土壤中的 CH4 生成,这主要是由于土壤变暖所致,而不是由于 SOC 可用性增加导致的解冻诱导的乙酸发酵预期增加。我们的研究结果表明,冬季降水增加将增加北极冻原的 CH4 源强度,但由此产生的对气候变化的正反馈将取决于积雪量增加或减少的地区与当前相比的平衡情况。