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Vertical profiles of CO\u3csub\u3e2\u3c/sub\u3e above eastern Amazonia suggest a net carbon flux to the atmosphere and balanced biosphere between 2000 and 2009

机译:亚马逊东部上空的CO \ u3csub \ u3e2 \ u3c / sub \ u3e垂直剖面显示2000年至2009年间大气净碳通量和平衡生物圈

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摘要

From 2000 until January 2010 vertical profiles were collected above eastern Amazonia to help determine regional-scale (∼105–106 km2) fluxes of carbon cycle-related greenhouse gases. Samples were collected aboard light aircraft between the surface and 4.3 km and a column integration technique was used to determine the CO2 flux. Measured CO2 profiles were differenced from the CO2 background determined from measurements in the tropical Atlantic. The observed annual flux between the coast and measurement sites was 0.40 ± 0.27 gC m−2 d−1 (90% confidence interval using a bootstrap analysis). The wet season (January–June) mean flux was 0.44 ± 0.38 gC m−2 d−1 (positive fluxes defined as a source to the atmosphere) and the dry season mean flux was 0.35 ± 0.17 gC m−2 d−1 (July–December). The observed flux variability is high, principally in the wet season. The influence of biomass burning has been removed using co-measured CO, and revealed the presence of a significant dry season sink. The annual mean vegetation flux, after the biomass burning correction, was 0.02 ± 0.27 gC m−2 d−1, and a clear sink was observed between August and November of −0.70 ± 0.21 gC m−2 d−1 where for all of the dry season it was −0.24 ± 0.17 gC m−2 d−1.
机译:从2000年到2010年1月,在亚马逊东部东部收集了垂直剖面,以帮助确定与碳循环有关的温室气体的区域规模通量(约105-106 km2)。在水面和4.3 km之间的一架轻型飞机上收集了样品,并使用柱积分技术确定了CO2通量。测得的二氧化碳分布与热带大西洋地区的二氧化碳背景不同。观测到的海岸和测量点之间的年通量为0.40±0.27 gC m-2 d-1(使用自举分析的置信区间为90%)。湿季(1月至6月)的平均通量为0.44±0.38 gC m-2 d-1(正向通量定义为大气源),而旱季的平均通量为0.35±0.17 gC m-2 d-1( 7月-12月)。观测到的通量变化很大,主要是在雨季。使用共同测量的CO消除了生物质燃烧的影响,并表明存在明显的旱季下沉。经过生物量燃烧校正后,年平均植被通量为0.02±0.27 gC m-2 d-1,并且在8月至11月之间观测到了一个清晰的汇,为-0.70±0.21 gC m-2 d-1。旱季为-0.24±0.17 gC m-2 d-1。

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