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Net carbon emissions from African biosphere dominate pan-tropical atmospheric CO2 signal

机译:非洲生物圈的净碳排放量占泛热带大气CO2信号的主导

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摘要

Tropical ecosystems are large carbon stores that are vulnerable to climate change. The sparseness of ground-based measurements has precluded verification of these ecosystems being a net annual source (+ve) or sink (−ve) of atmospheric carbon. We show that two independent satellite data sets of atmospheric carbon dioxide (CO2), interpreted using independent models, are consistent with the land tropics being a net annual carbon emission of (medianminimummaximum) 1.03-0.20+1.73 and 1.60+1.39+2.11 petagrams (PgC) in 2015 and 2016, respectively. These pan-tropical estimates reflect unexpectedly large net emissions from tropical Africa of 1.48+0.80+1.95 PgC in 2015 and 1.65+1.14+2.42 PgC in 2016. The largest carbon uptake is over the Congo basin, and the two loci of carbon emissions are over western Ethiopia and western tropical Africa, where there are large soil organic carbon stores and where there has been substantial land use change. These signals are present in the space-borne CO2 record from 2009 onwards.
机译:热带生态系统是易受气候变化影响的大型碳库。地面测量的稀疏性阻止了对这些生态系统是大气碳的净年源(+ ve)或汇(-ve)的验证。我们显示,使用独立模型解释的两个独立的大气二氧化碳(CO2)卫星数据集与陆地热带一致,即每年的净碳排放量为 中位数 最小 最大 < / mrow> 1.0 3 - 0.20 + 1.73 1.6 0 + 1.39 + 2.11 花瓣(分别于2015年和2016年发布。这些泛热带估算值反映了 1.4 8 + 0.80 + 1.95 PgC在2015年和 1.6 5 + < /mo>1.14 + 2.42 PgC。最大的碳吸收量是在刚果盆地上,并且两个碳排放位点是在埃塞俄比亚西部和热带非洲西部,那里土壤有机碳储量很大,土地使用发生了巨大变化。从2009年起,这些信号存在于星载CO2记录中。

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