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Ecosystem carbon transit versus turnover times in response to climate warming and rising atmospheric COsub2/sub concentration

机译:气候变暖和大气CO 2 浓度升高对生态系统碳迁移与周转时间的影响

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摘要

Ecosystem carbon (C) transit time is a critical diagnostic parameter to characterize land C sequestration. This parameter has different variants in the literature, including a commonly used turnover time. However, we know little about how different transit time and turnover time are in representing carbon cycling through multiple compartments under a non-steady state. In this study, we estimate both C turnover time as defined by the conventional stock over flux and mean C transit time as defined by the mean age of C mass leaving the system. We incorporate them into the Community Atmosphere Biosphere Land Exchange (CABLE) model to estimate C turnover time and transit time in response to climate warming and rising atmospheric [COsub2/sub]. Modelling analysis shows that both C turnover time and transit time increase with climate warming but decrease with rising atmospheric [COsub2/sub]. Warming increases C turnover time by 2.4?years and transit time by 11.8?years in 2100 relative to that at steady state in 1901. During the same period, rising atmospheric [COsub2/sub] decreases C turnover time by 3.8?years and transit time by 5.5?years. Our analysis shows that 65 % of the increase in global mean C transit time with climate warming results from the depletion of fast-turnover C pool. The remaining 35 % increase results from accompanied changes in compartment C age structures. Similarly, the decrease in mean C transit time with rising atmospheric [COsub2/sub] results approximately equally from replenishment of C into fast-turnover C pool and subsequent decrease in compartment C age structure. Greatly different from the transit time, the turnover time, which does not account for changes in either C age structure or composition of respired C, underestimated impacts of warming and rising atmospheric [COsub2/sub] on C diagnostic time and potentially led to deviations in estimating land C sequestration in multi-compartmental ecosystems.
机译:生态系统碳(C)的运输时间是表征土地固碳的关键诊断参数。该参数在文献中有不同的变体,包括常用的周转时间。但是,我们对于在非稳态下通过多个车厢的碳循环表现出不同的运输时间和周转时间知之甚少。在这项研究中,我们估算了由常规存量相对于通量定义的C周转时间,以及由离开系统的C质的平均年龄定义的平均C传递时间。我们将它们合并到社区大气生物圈土地交换(CABLE)模型中,以估算响应气候变暖和大气层[CO 2 ]的碳周转时间和运输时间。建模分析表明,随着气候变暖,碳的周转时间和穿越时间均随大气[CO 2 ]的增加而减少。相对于1901年的稳定状态,升温使2100年的C转换时间增加了2.4?年,传输时间增加了11.8?年。在同一时期,大气中[CO 2 ]的升高使C转换时间减少了3.8年,运输时间缩短5.5年。我们的分析表明,随着气候变暖,全球平均C过渡时间增加的65%来自快速周转的C库的耗尽。剩下的35%的增加是由于车厢C年龄结构的伴随变化所致。同样,随着大气中[CO 2 ]的升高,平均C穿越时间的减少大致等同地归因于将C补充到快速周转的C池中以及随后车厢C年龄结构的减少。与转换时间有很大不同的是,转换时间没有考虑C年龄结构或呼吸C组成的变化,但低估了气候变暖和大气[CO 2 ]对C诊断时间的影响并可能导致在多隔室生态系统中估算土地固存量方面的偏差。

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