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早期地球对由二氧化碳云导致的不可逆冰川作用的敏感性。

Susceptibility of the early Earth to irreversible glaciation caused by carbon dioxide clouds.

作者信息

Caldeira K, Kasting J F

机构信息

Department of Geosciences, The Pennsylvania State University, University Park 16802, USA.

出版信息

Nature. 1992 Sep 17;359:226-8. doi: 10.1038/359226a0.

Abstract

Simple energy-balance climate models of the Budyko/Sellers type 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 history 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 warm. 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 Mars. 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.

摘要

布迪科/塞勒斯类型的简单能量平衡气候模型预测,太阳辐射输出量小幅下降(2%-5%)可能导致地球出现失控的冰川作用。但在地球历史早期,太阳通量低25%-30%时显然并未导致这种结果。目前一种备受青睐的解释是,较高的火山排气速率和/或较慢的硅酸盐风化速率导致二氧化碳分压较高,从而产生了足够大的温室效应使地球保持温暖。然而,这并没有解决气候稳定性问题,因为正如我们在此所论证的,海洋结冰的速度比二氧化碳在大气中积累的速度要快得多。如果在遥远的过去太阳光度较低时发生过这种短暂的全球冰川作用,由于形成了高反射性的二氧化碳云,类似于早期火星气候模拟中遇到的情况,那么它可能是不可逆转的。我们对早期地球的模拟,考虑了此类云形成的可能性,结果表明,如果地球在其历史的第一阶段没有保持温暖,那么今天它可能就不适宜居住了。

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