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DOI10.1126/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
ISSN0036-8075
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
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
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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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