Measurement of CO2 exchange between Boreal forest and the atmosphere.

T. A. Black, D. Gaumont-Guay, R. Jassal, B. Amiro, P. Jarvis, S. Gower, F. Kelliher, A. Dunn, S. Wofsy
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引用次数: 28

Abstract

The Boreal forest is the world's second largest forested biome occupying the circumpolar region between 50 degrees N and 70 degrees N. This heterogeneous biome stores about 25% of all terrestrial carbon. We have reviewed EC measurements of CO2 exchange between the atmosphere and Boreal forests, and assessed progress in understanding the controlling processes. We have assessed net ecosystem productivity, the net balance between net primary productivity and heterotrophic respiration, measured using the EC method, for 38 Boreal forest sites. Gross ecosystem productivity has been estimated by adding day-time EC-measured CO2 fluxes to respiration estimated from night-time relationships between respiration and temperature. Maximum midday values of gross ecosystem productivity vary from 33 pmol m(-2) s(-1) for aspen to 6 micromol m(-2) s(-1) for larch stands. Long-term EC flux measurements, ongoing at nine Boreal sites, have shown the strong impact of spring weather and growing season water balance on annual net ecosystem productivity. Estimation of net biome production, incorporating the effects of disturbance resulting from forest fires and logging, has progressed significantly in recent years. After disturbance, summer measurements in Boreal chronosequences suggest that it takes about 10 years before growing season carbon uptake offsets the decomposition emissions. Small-scale exchange rate measurements using chambers and manipulative experiments such as stem girdling and soil heating help to understand the processes and mechanisms playing major roles in the carbon balance of terrestrial ecosystems. Aircraft EC flux measurements, convective boundary layer carbon budgets, and (13)C/12C changes in the atmosphere play an important role in validating estimates of regional carbon exchange based on scaled up EC measurements. Atmospheric inverse models are an important approach to studying regional and global carbon balance but need further improvement to yield reliable quantitative results.
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测量北方森林与大气之间的二氧化碳交换。
北方森林是世界上第二大森林生物群落,位于北纬50度至北纬70度之间的环极地区,这种异质性生物群落储存了大约25%的陆地碳。我们回顾了欧共体对大气与北方森林之间二氧化碳交换的测量,并评估了在了解控制过程方面取得的进展。我们评估了38个北方针叶林样地的净生态系统生产力,即净初级生产力和异养呼吸之间的净平衡,使用EC方法测量。总生态系统生产力是通过将白天ec测量的二氧化碳通量加入由夜间呼吸和温度之间的关系估算的呼吸作用中来估算的。总生态系统生产力的最大正午值从杨树的33 μ mol m(-2) s(-1)到落叶松林的6 μ mol m(-2) s(-1)不等。在9个北纬地区站点进行的长期EC通量测量显示,春季天气和生长期水分平衡对年净生态系统生产力有强烈影响。考虑到森林火灾和伐木造成的干扰的影响,对净生物群落产量的估计近年来取得了重大进展。干扰后,北方森林夏季时间序列的测量结果表明,生长季碳吸收需要大约10年才能抵消分解排放。利用室和可操作实验(如茎束和土壤加热)进行的小规模汇率测量有助于了解在陆地生态系统碳平衡中起主要作用的过程和机制。飞机EC通量测量、对流边界层碳收支和大气(13)C/12C变化在验证基于放大EC测量的区域碳交换估算中发挥了重要作用。大气反演模型是研究区域和全球碳平衡的重要方法,但需要进一步改进才能得到可靠的定量结果。
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