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DOI | 10.1126/science.274.5291.1346 |
Oceanic carbon dioxide uptake in a model of century-scale global warming | |
Sarmiento J.L.; Le Quéré C. | |
发表日期 | 1996 |
ISSN | 0036-8075 |
起始页码 | 1346 |
结束页码 | 1350 |
卷号 | 274期号:5291 |
英文摘要 | In a model of ocean-atmosphere interaction that excluded biological processes, the oceanic uptake of atmospheric carbon dioxide (CO2) was substantially reduced in scenarios involving global warming relative to control scenarios. The primary reason for the reduced uptake was the weakening or collapse of the ocean thermohaline circulation. Such a large reduction in this ocean uptake would have a major impact on the future growth rate of atmospheric CO2. Model simulations that include a simple representation of biological processes show a potentially large offsetting effect resulting from the downward flux of biogenic carbon. However, the magnitude of the offset is difficult to quantify with present knowledge. |
英文关键词 | carbon dioxide; organic matter; article; atmosphere; climate; controlled study; environmental temperature; greenhouse effect; priority journal; sea; air-sea interaction; air/sea interaction; atmosphere/ocean interaction; carbon dioxide; climate change; global warming; model; oceanic uptake |
语种 | 英语 |
来源期刊 | Science
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/245343 |
作者单位 | Prog. in Atmosph. and Oceanic Sci., Princeton University, Princeton, NJ 08544, United States |
推荐引用方式 GB/T 7714 | Sarmiento J.L.,Le Quéré C.. Oceanic carbon dioxide uptake in a model of century-scale global warming[J],1996,274(5291). |
APA | Sarmiento J.L.,&Le Quéré C..(1996).Oceanic carbon dioxide uptake in a model of century-scale global warming.Science,274(5291). |
MLA | Sarmiento J.L.,et al."Oceanic carbon dioxide uptake in a model of century-scale global warming".Science 274.5291(1996). |
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