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Primary Discussion of a Carbon Sink in the Oceans

查看全文 作  者:MA [1,2]Caihua;YOU [3,2]Kui;JI [1]Dechun;MA [1]Weiwei;LI [1]Fengqi 高影响力作者 机构地区:[1]Ocean University of China;[2]Woods Hole Oceanographic Institution;[3]Dalian University of Technology高影响力机构 出  处:《Journal of Ocean University of China》索引2015年第14卷第2期,共9页高影响力期刊 基  金:Financial support was provided by the National Natural Science Foundation of China (41106094);the Department of Science and Technology Project (BS2010NY030) 摘  要:As a consequence of global warming and rising sea levels, the oceans are becoming a matter of concern for more and more people because these changes will impact the growth of living organisms as well as people's living standards. In particular, it is extremely important that the oceans absorb massive amounts of carbon dioxide. This paper takes a pragmatic approach to analyzing the oceans with respect to the causes of discontinuities in oceanic variables of carbon dioxide sinks. We report on an application of chemical, physical and biological methods to analyze the changes of carbon dioxide in oceans. Based on the relationships among the oceans, land, atmosphere and sediment with respect to carbon dioxide, the foundation of carbon dioxide in shell-building and ocean acidification, the changes in carbon dioxide in the oceans and their impact on climate change, and so on, a vital conclusion can be drawn from this study. Specifically, under the condition that the oceans are not disturbed by external forces, the oceans are a large carbon dioxide sink. The result can also be inferred by the formula: C=A-B and G=E+F when the marine ecosystem can keep a natural balance and the amount of carbon dioxide emission is limited within the carrying capacity of the oceans. 关 键 词:二氧化碳排放量 海洋生态系统 全球气候变暖 气候变化影响 海平面上升 不连续性 生物方法 自然平衡
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