碳循环
生物地球化学循环
地球系统科学
环境科学
地球科学
大气(单位)
自然(考古学)
土(古典元素)
生态系统
碳纤维
陆地生态系统
天体生物学
大气科学
生态学
气象学
地理
计算机科学
地质学
生物
物理
考古
算法
复合数
数学物理
作者
Paul G. Falkowski,Robert J. Scholes,E. Boyle,Josep G. Canadell,Donald E. Canfield,James J. Elser,Nicolas Gruber,Kathy Hibbard,Peter Högberg,Sune Linder,Fred T. Mackenzie,Berrien Moore,Thomas F. Pedersen,Yair Rosenthal,Sybil P. Seitzinger,Victor Smetacek,Will Steffen
出处
期刊:Science
[American Association for the Advancement of Science (AAAS)]
日期:2000-10-13
卷期号:290 (5490): 291-296
被引量:1830
标识
DOI:10.1126/science.290.5490.291
摘要
Motivated by the rapid increase in atmospheric CO 2 due to human activities since the Industrial Revolution, several international scientific research programs have analyzed the role of individual components of the Earth system in the global carbon cycle. Our knowledge of the carbon cycle within the oceans, terrestrial ecosystems, and the atmosphere is sufficiently extensive to permit us to conclude that although natural processes can potentially slow the rate of increase in atmospheric CO 2 , there is no natural “savior” waiting to assimilate all the anthropogenically produced CO 2 in the coming century. Our knowledge is insufficient to describe the interactions between the components of the Earth system and the relationship between the carbon cycle and other biogeochemical and climatological processes. Overcoming this limitation requires a systems approach.
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