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Quantifying spatially and temporally explicit CO2 fertilization effects on global terrestrial ecosystem carbon dynamics

机译:量化时空明确的 CO 2 施肥对全球陆地生态系统碳动态的影响

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Current terrestrial ecosystem models are usually driven with global average annual atmospheric carbon dioxide ( CO _(2)) concentration data at the global scale. However, high‐precision CO _(2) measurement from eddy flux towers showed that seasonal, spatial surface atmospheric CO _(2) concentration differences were as large as 35 ppmv and the site‐level tests indicated that the CO _(2) variation exhibited different effects on plant photosynthesis. Here we used a process‐based ecosystem model driven with two spatially and temporally explicit CO _(2) data sets to analyze the atmospheric CO _(2) fertilization effects on the global carbon dynamics of terrestrial ecosystems from 2003 to 2010. Our results demonstrated that CO _(2) seasonal variation had a negative effect on plant carbon assimilation, while CO _(2) spatial variation exhibited a positive impact. When both CO _(2) seasonal and spatial effects were considered, global gross primary production and net ecosystem production were 1.7?Pg?C·yr~(?1) and 0.08?Pg?C·yr~(?1) higher than the simulation using uniformly distributed CO _(2) data set and the difference was significant in tropical and temperate evergreen broadleaf forest regions. This study suggests that the CO _(2) observation network should be expanded so that the realistic CO _(2) variation can be incorporated into the land surface models to adequately account for CO _(2) fertilization effects on global terrestrial ecosystem carbon dynamics.
机译:当前的陆地生态系统模型通常由全球规模的全球平均年度大气二氧化碳(CO_(2))浓度数据驱动。但是,通过涡流塔进行的高精度CO _(2)测量表明,季节性,空间表面大气CO _(2)浓度差高达35 ppmv,现场测试表明,CO _(2)的变化表现出对植物光合作用的不同影响。在这里,我们使用了基于过程的生态系统模型,该模型基于两个在空间和时间上都明确的CO _(2)数据集来分析2003年至2010年大气CO _(2)施肥对陆地生态系统全球碳动态的影响。我们的结果证明了CO _(2)的季节变化对植物碳同化有负面影响,而CO _(2)的空间变化表现出正影响。当同时考虑CO _(2)的季节和空间影响时,全球初级总生产量和生态系统净产量比分别高1.7?Pg?C·yr〜(?1)和0.08?Pg?C·yr〜(?1)。使用均匀分布的CO _(2)数据集进行的模拟,在热带和温带常绿阔叶林地区的差异非常显着。这项研究表明,应扩大CO _(2)观测网络,以便可以将现实的CO _(2)变化纳入陆地表面模型,以充分考虑CO _(2)施肥对全球陆地生态系统碳动态的影响。 。

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