Effects of increased CO2 concentrations on surface temperature of the early Earth

One of the major riddles of terrestrial evolution concerns the history of the Earth's surface temperature. Present models of solar evolution indicate that the luminosity was about 25% smaller at the time of formation of the Solar System 1 . This factor alone would have caused the Earth's s...

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Bibliographic Details
Published in:Nature (London) 1983-01, Vol.301 (5895), p.53-55
Main Authors: Kuhn, William R., Kasting, James F.
Format: Article
Language:English
Subjects:
Earth sciences
Earth, ocean, space
Exact sciences and technology
Geochemistry
Geochemistry: general, methodology, regional studies
Humanities and Social Sciences
letter
multidisciplinary
Science
Science (multidisciplinary)
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Summary:One of the major riddles of terrestrial evolution concerns the history of the Earth's surface temperature. Present models of solar evolution indicate that the luminosity was about 25% smaller at the time of formation of the Solar System 1 . This factor alone would have caused the Earth's surface temperature to be below freezing, yet the geological record indicates that water has flowed on the surface since at least 3,800 Myr ago 2 . Enhanced levels of CO 2 in the atmosphere could have provided the necessary warming to maintain the temperature above freezing. Increased tectonic activity, and a decrease in solubility of CO 2 in the oceans, rock weathering, and sediment deposition are processes that have been suggested for these larger amounts of CO 2 . We show here that large CO 2 concentrations are necessary to maintain the early Earth's surface temperature at approximately today's level. If there were a thousand tunes the present atmospheric level (PAL) of CO 2 in the atmosphere, the temperature would be 292K, while a 100-fold increase in CO 2 concentration yields 284K. The surface warming is highly dependent on the amount of water vapour and clouds, both of which we have little knowledge of for this very early time in the Earth's history.
ISSN:0028-0836
1476-4687
DOI:10.1038/301053a0