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内陆水体的全球二氧化碳排放量。

Global carbon dioxide emissions from inland waters.

机构信息

Yale School of Forestry and Environmental Studies, 195 Prospect Street, New Haven, Connecticut 06511, USA.

出版信息

Nature. 2013 Nov 21;503(7476):355-9. doi: 10.1038/nature12760.

Abstract

Carbon dioxide (CO2) transfer from inland waters to the atmosphere, known as CO2 evasion, is a component of the global carbon cycle. Global estimates of CO2 evasion have been hampered, however, by the lack of a framework for estimating the inland water surface area and gas transfer velocity and by the absence of a global CO2 database. Here we report regional variations in global inland water surface area, dissolved CO2 and gas transfer velocity. We obtain global CO2 evasion rates of 1.8(+0.25)(-0.25)  petagrams of carbon (Pg C) per year from streams and rivers and 0.32(+0.52)(-0.26)  Pg C yr(-1) from lakes and reservoirs, where the upper and lower limits are respectively the 5th and 95th confidence interval percentiles. The resulting global evasion rate of 2.1 Pg C yr(-1) is higher than previous estimates owing to a larger stream and river evasion rate. Our analysis predicts global hotspots in stream and river evasion, with about 70 per cent of the flux occurring over just 20 per cent of the land surface. The source of inland water CO2 is still not known with certainty and new studies are needed to research the mechanisms controlling CO2 evasion globally.

摘要

二氧化碳(CO2)从内陆水体向大气中的转移,称为 CO2 逸散,是全球碳循环的一个组成部分。然而,由于缺乏估算内陆水表面积和气体转移速度的框架,以及缺乏全球 CO2 数据库,全球 CO2 逸散量的估算受到了阻碍。在这里,我们报告了全球内陆水表面积、溶解 CO2 和气体转移速度的区域变化。我们得出,全球溪流和河流每年的 CO2 逸散率为 1.8(+0.25)(-0.25) PgC,湖泊和水库的 CO2 逸散率为 0.32(+0.52)(-0.26) PgCyr(-1),其中上限和下限分别为第 5 和第 95 置信区间百分位数。由于溪流和河流的逸散率较高,因此得出的全球逸散率为 2.1 PgC yr(-1),高于之前的估计。我们的分析预测了溪流和河流逸散的全球热点,其中约 70%的通量仅发生在 20%的陆地表面上。内陆水 CO2 的来源仍不能确定,需要进行新的研究来研究全球 CO2 逸散的控制机制。

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