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Time scales and ratios of climate forcing due to thermal versus carbon dioxide emissions from fossil fuels
Author(s) -
Zhang Xiaochun,
Caldeira Ken
Publication year - 2015
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1002/2015gl063514
Subject(s) - radiative forcing , fossil fuel , environmental science , carbon dioxide , atmosphere (unit) , atmospheric sciences , combustion , greenhouse gas , forcing (mathematics) , radiative transfer , methane , carbon fibers , climate change , meteorology , chemistry , geology , materials science , physics , oceanography , organic chemistry , quantum mechanics , composite number , composite material
The Earth warms both when fossil fuel carbon is oxidized to carbon dioxide and when greenhouse effect of carbon dioxide inhibits longwave radiation from escaping to space. Various important time scales and ratios comparing these two climate forcings have not previously been quantified. For example, the global and time‐integrated radiative forcing from burning a fossil fuel exceeds the heat released upon combustion within 2 months. Over the long lifetime of CO 2 in the atmosphere, the cumulative CO 2 ‐radiative forcing exceeds the amount of energy released upon combustion by a factor >100,000. For a new power plant, the radiative forcing from the accumulation of released CO 2 exceeds the direct thermal emissions in less than half a year. Furthermore, we show that the energy released from the combustion of fossil fuels is now about 1.71% of the radiative forcing from CO 2 that has accumulated in the atmosphere as a consequence of historical fossil fuel combustion.