SUSCEPTIBILITY OF THE EARLY EARTH TO IRREVERSIBLE GLACIATION CAUSED BY CARBON-DIOXIDE CLOUDS

被引:161
作者
CALDEIRA, K [1 ]
KASTING, JF [1 ]
机构
[1] PENN STATE UNIV,DEPT GEOSCI,UNIV PK,PA 16802
关键词
D O I
10.1038/359226a0
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
SIMPLE energy-balance climate models of the Budyko/Sellers type1,2 predict that a small (2-5%) decrease in solar output could result in runaway glaciation on the Earth. But solar fluxes 25-30% lower early in the Earth's history3,4 apparently did not lead to this result. One currently favoured explanation is that high partial pressures of carbon dioxide, caused by higher volcanic outgassing rates and/or slower rates of silicate weathering, created a large enough greenhouse effect to keep the planet warm5-7. This does not resolve the problem of climate stability, however, because as we argue here, the oceans can freeze much more quickly than CO2 can accumulate in the atmosphere. Had such a transient global glaciation occurred in the distant past when solar luminosity was low, it might have been irreversible because of the formation of highly reflective CO2 clouds, similar to those encountered in climate simulations of early Mars8. Our simulations of the early Earth, incorporating the possible formation of such clouds, suggest that the Earth might not be habitable today had it not been warm during the first part of its history.
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页码:226 / 228
页数:3
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