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首页> 外文期刊>Global change biology >Rain events decrease boreal peatland net CO2 uptake through reduced light availability
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Rain events decrease boreal peatland net CO2 uptake through reduced light availability

机译:降雨事件通过减少可用光量减少了北方泥炭地净二氧化碳吸收量

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Boreal peatlands store large amounts of carbon, reflecting their important role in the global carbon cycle. The short-term exchange and the long-term storage of atmospheric carbon dioxide (CO2) in these ecosystems are closely associated with the permanently wet surface conditions and are susceptible to drought. Especially, the single most important peat forming plant genus, Sphagnum, depends heavily on surface wetness for its primary production. Changes in rainfall patterns are expected to affect surface wetness, but how this transient rewetting affects net ecosystem exchange of CO2 (NEE) remains unknown. This study explores how the timing and characteristics of rain events during photosynthetic active periods, that is daytime, affect peatland NEE and whether rain event associated changes in environmental conditions modify this response (e.g. water table, radiation, vapour pressure deficit, temperature). We analysed an 11-year time series of half-hourly eddy covariance and meteorological measurements from Degero Stormyr, a boreal peatland in northern Sweden. Our results show that daytime rain events systematically decreased the sink strength of peatlands for atmospheric CO2. The decrease was best explained by rain associated reduction in light, rather than by rain characteristics or drought length. An average daytime growing season rain event reduced net ecosystem CO2 uptake by 0.23-0.54gCm(-2). On an annual basis, this reduction of net CO2 uptake corresponds to 24% of the annual net CO2 uptake (NEE) of the study site, equivalent to a 4.4% reduction of gross primary production (GPP) during the growing season. We conclude that reduced light availability associated with rain events is more important in explaining the NEE response to rain events than rain characteristics and changes in water availability. This suggests that peatland CO2 uptake is highly sensitive to changes in cloud cover formation and to altered rainfall regimes, a process hitherto largely ignored.
机译:北方泥炭地存储大量碳,这反映了它们在全球碳循环中的重要作用。这些生态系统中的大气二氧化碳(CO2)的短期交换和长期存储与永久湿润的表面条件密切相关,并且容易受到干旱的影响。尤其是,最重要的一个形成泥炭的植物植物泥炭藓主要依赖表面湿润度。降雨模式的变化有望影响地表湿度,但是这种暂时性再润湿如何影响生态系统净二氧化碳交换量(NEE)仍然未知。这项研究探讨了在光合作用活动期间(即白天)降雨事件的时间和特征如何影响泥炭地NEE,以及与降雨事件相关的环境条件是否会改变这种响应(例如地下水位,辐射,蒸气压赤字,温度)。我们分析了Degero Stormyr(瑞典北部的一个北部泥炭地)的半小时涡流协方差和气象测量结果的11年时间序列。我们的结果表明,白天的降雨事件会系统地降低泥炭地的大气CO2汇强度。减少的最好解释是与降雨有关的光照减少,而不是由降雨特性或干旱时间长短引起的。平均白天的生长期降雨事件使净生态系统二氧化碳吸收减少了0.23-0.54gCm(-2)。从每年的角度来看,这种二氧化碳净吸收量的减少相当于研究地点年度二氧化碳净吸收量(NEE)的24%,相当于生长季节总初级生产量(GPP)减少4.4%。我们得出的结论是,与降雨特征和供水量的变化相比,与降雨事件有关的光利用率降低在解释NEE对降雨事件的响应方面更为重要。这表明泥炭地对二氧化碳的吸收对云层形成的变化和降雨方式的变化高度敏感,这一过程迄今为止一直被忽略。

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