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Evaluating Northern Hemisphere Growing Season Net Carbon Flux in Climate Models Using Aircraft Observations

机译:利用飞机观测评估气候模型中北半球生长季净碳通量

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Abstract Understanding terrestrial ecosystems and their response to anthropogenic climate change requires quantification of land‐atmosphere carbon exchange. However, top‐down and bottom‐up estimates of large‐scale land‐atmosphere fluxes, including the northern extratropical growing season net flux (GSNF), show significant discrepancies. We developed a data‐driven metric for the GSNF using atmospheric carbon dioxide concentration observations collected during the High‐Performance Instrumented Airborne Platform for Environmental Research Pole‐to‐Pole Observations and Atmospheric Tomography Mission flight campaigns. This aircraft‐derived metric is bias‐corrected using three independent atmospheric inversion systems. We estimate the northern extratropical GSNF to be 5.7 ± 0.3 Pg C and use it to evaluate net biosphere productivity from the Coupled Model Intercomparison Project phase 5 and 6 (CMIP5 and CMIP6) models. While the model‐to‐model spread in the GSNF has decreased in the CMIP6 models relative to that of the CMIP5 models, there is still disagreement on the magnitude and timing of seasonal carbon uptake with most models underestimating the GSNF and overestimating the length of the growing season relative to the observations. We also use an emergent constraint approach to estimate annual northern extratropical gross primary productivity to be 56 ± 17 Pg C, heterotrophic respiration to be 25 ± 13 Pg C, and net primary productivity to be 28 ± 12 Pg C. The flux inferred from these aircraft observations provides an additional constraint on large‐scale gross fluxes in prognostic Earth system models that may ultimately improve our ability to accurately predict carbon‐climate feedbacks.
机译:摘要 了解陆地生态系统及其对人为气候变化的响应需要对陆地-大气碳交换进行量化。然而,自上而下和自下而上对大尺度陆地-大气通量的估计,包括北部温带生长季净通量(GSNF),显示出显著的差异。我们利用高性能仪器化机载平台的环境研究、极对极观测和大气层层扫描任务飞行活动期间收集的大气二氧化碳浓度观测数据,为 GSNF 开发了一个数据驱动的指标。这个源自飞机的指标使用三个独立的大气逆温系统进行偏差校正。我们估计北部温带GSNF为5.7 ± 0.3 Pg C,并用它来评估耦合模式比较项目第5和第6阶段(CMIP5和CMIP6)模型的净生物圈生产力。虽然与CMIP5模式相比,CMIP6模式的GSNF模型间分布有所减小,但对季节性碳吸收的规模和时间仍存在分歧,大多数模式低估了GSNF,高估了相对于观测值的生长季节长度。我们还使用紧急约束方法估计年北温带总初级生产力为56 ± 17 Pg C,异养呼吸为25 ± 13 Pg C,净初级生产力为28 ± 12 Pg C。从这些飞机观测中推断出的通量为预测地球系统模型中的大规模总通量提供了额外的限制,这可能最终提高我们准确预测碳气候反馈的能力。

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