温室气体
温室气体清除
环境科学
一氧化二氮
化石燃料
气候变化
甲烷
无组织排放
二氧化碳
全球变暖
温室效应
环境保护
减缓气候变化
废物管理
化学
生态学
生物
工程类
有机化学
作者
S. A. Montzka,E. J. Dlugokencky,J. H. Butler
出处
期刊:Nature
[Nature Portfolio]
日期:2011-08-02
卷期号:476 (7358): 43-50
被引量:1227
摘要
Earth's climate is warming as a result of anthropogenic emissions of greenhouse gases, particularly carbon dioxide (CO(2)) from fossil fuel combustion. Anthropogenic emissions of non-CO(2) greenhouse gases, such as methane, nitrous oxide and ozone-depleting substances (largely from sources other than fossil fuels), also contribute significantly to warming. Some non-CO(2) greenhouse gases have much shorter lifetimes than CO(2), so reducing their emissions offers an additional opportunity to lessen future climate change. Although it is clear that sustainably reducing the warming influence of greenhouse gases will be possible only with substantial cuts in emissions of CO(2), reducing non-CO(2) greenhouse gas emissions would be a relatively quick way of contributing to this goal.
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