Black T Andrew, Gaumont-Guay David, Jassal Rachhpal S, Amiro Brian D, Jarvis Paul G, Gower Stith T, Kelliher Frank M, Dunn Allison, Wofsy Steven C
Department of Agricultural Sciences, University of British Columbia, Vancouver, Canada.
SEB Exp Biol Ser. 2005:151-85.
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.
北方森林是世界第二大森林生物群落,占据北纬50度至70度之间的环极地区。这个异质生物群落储存了约25%的陆地碳。我们回顾了大气与北方森林之间二氧化碳交换的涡度相关测量,并评估了在理解控制过程方面取得的进展。我们使用涡度相关方法评估了38个北方森林站点的生态系统净生产力,即净初级生产力与异养呼吸之间的净平衡。通过将白天涡度相关测量的二氧化碳通量与根据夜间呼吸与温度关系估算的呼吸量相加,估算了生态系统总生产力。生态系统总生产力的最大中午值从山杨的33 pmol m(-2) s(-1)到落叶松林的6 μmol m(-2) s(-1)不等。在九个北方站点进行的长期涡度相关通量测量表明,春季天气和生长季水分平衡对年度生态系统净生产力有强烈影响。近年来,在纳入森林火灾和伐木造成的干扰影响的生物群落净生产估算方面取得了显著进展。干扰后,北方森林演替序列的夏季测量表明,生长季碳吸收抵消分解排放大约需要10年时间。使用气室进行的小规模交换率测量以及诸如茎环割和土壤加热等操纵性实验有助于理解在陆地生态系统碳平衡中起主要作用的过程和机制。飞机涡度相关通量测量、对流边界层碳收支以及大气中(13)C/12C的变化在验证基于放大涡度相关测量的区域碳交换估算方面发挥着重要作用。大气反演模型是研究区域和全球碳平衡的重要方法,但需要进一步改进以获得可靠的定量结果。