Atmospheric carbon dioxide and the long-term control of the Earth's climate

A CO<sub>2</sub>-weathering model has been used to explore the possible evolution of the Earth's climate as the Sun steadily brightened throughout geologic time. The results of the model calculations can be described in terms of three, qualitatively different, &quot;Megaclima...

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Main Authors: J. H. Carver, I. M. Vardavas
Format: Article
Language:English
Published: Copernicus Publications 1995-07-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/13/782/1995/angeo-13-782-1995.pdf
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spelling doaj-c4aa5fa938af4f339ebc800572f145fc2020-11-24T23:24:37ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05761995-07-011378279010.1007/s00585-995-0782-8Atmospheric carbon dioxide and the long-term control of the Earth's climateJ. H. CarverI. M. VardavasA CO<sub>2</sub>-weathering model has been used to explore the possible evolution of the Earth's climate as the Sun steadily brightened throughout geologic time. The results of the model calculations can be described in terms of three, qualitatively different, &quot;Megaclimates&quot;. Mega-climate 1 resulted from a period of rapid outgassing in the early Archean, with high, but declining, temperatures caused by the small weathering rates on a largely water-covered planet. Mega-climate 2 began about 3 Gyear ago as major continental land masses developed, increasing the weathering rate in the early Proterozoic and thereby depleting the atmospheric CO<sub>2</sub> concentration. This process produced the first Precambrian glaciations about 2.3 Gyear ago. During Mega-climate 2, evolutionary biological processes increased the surface weatherability in incremental steps and plate tectonics modulated the CO<sub>2</sub> outgassing rate with an estimated period of 150 Myear (approximately one-half the period for the formation and breakup of super continents). Throughout Mega-climate 2 the surface temperature was controlled by variations in the atmospheric CO<sub>2</sub> level allowing transitions between glacial and non-glacial conditions. The results of the model for Mega-climate 2 are in agreement with the occurrence (and absence) of glaciations in the geologic record. Extending the model to the future suggests that CO<sub>2</sub> control of the Earth's temperature will no longer be able to compensate for a solar flux that continues to increase. The present level of atmospheric CO<sub>2</sub> is so small that further reduction in CO<sub>2</sub> cannot prevent the Earth from experiencing Mega-climate 3 with steadily increasing surface temperatures caused by the continued brightening of the Sun. During Mega-climate 3, the main danger to the biosphere would come not from an increasing temperature but from a decreasing (rather than an increasing) CO<sub>2</sub> level which could, in time, fall below 0.5 PAL, causing serious damage to the biosphere. Fortunately, the rates of change due to solar brightening are slow enough that Mega-climate 3 appears to pose no threat to the biosphere for the next 0.5-2 Gyear.https://www.ann-geophys.net/13/782/1995/angeo-13-782-1995.pdf
collection DOAJ
language English
format Article
sources DOAJ
author J. H. Carver
I. M. Vardavas
spellingShingle J. H. Carver
I. M. Vardavas
Atmospheric carbon dioxide and the long-term control of the Earth's climate
Annales Geophysicae
author_facet J. H. Carver
I. M. Vardavas
author_sort J. H. Carver
title Atmospheric carbon dioxide and the long-term control of the Earth's climate
title_short Atmospheric carbon dioxide and the long-term control of the Earth's climate
title_full Atmospheric carbon dioxide and the long-term control of the Earth's climate
title_fullStr Atmospheric carbon dioxide and the long-term control of the Earth's climate
title_full_unstemmed Atmospheric carbon dioxide and the long-term control of the Earth's climate
title_sort atmospheric carbon dioxide and the long-term control of the earth's climate
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 1995-07-01
description A CO<sub>2</sub>-weathering model has been used to explore the possible evolution of the Earth's climate as the Sun steadily brightened throughout geologic time. The results of the model calculations can be described in terms of three, qualitatively different, &quot;Megaclimates&quot;. Mega-climate 1 resulted from a period of rapid outgassing in the early Archean, with high, but declining, temperatures caused by the small weathering rates on a largely water-covered planet. Mega-climate 2 began about 3 Gyear ago as major continental land masses developed, increasing the weathering rate in the early Proterozoic and thereby depleting the atmospheric CO<sub>2</sub> concentration. This process produced the first Precambrian glaciations about 2.3 Gyear ago. During Mega-climate 2, evolutionary biological processes increased the surface weatherability in incremental steps and plate tectonics modulated the CO<sub>2</sub> outgassing rate with an estimated period of 150 Myear (approximately one-half the period for the formation and breakup of super continents). Throughout Mega-climate 2 the surface temperature was controlled by variations in the atmospheric CO<sub>2</sub> level allowing transitions between glacial and non-glacial conditions. The results of the model for Mega-climate 2 are in agreement with the occurrence (and absence) of glaciations in the geologic record. Extending the model to the future suggests that CO<sub>2</sub> control of the Earth's temperature will no longer be able to compensate for a solar flux that continues to increase. The present level of atmospheric CO<sub>2</sub> is so small that further reduction in CO<sub>2</sub> cannot prevent the Earth from experiencing Mega-climate 3 with steadily increasing surface temperatures caused by the continued brightening of the Sun. During Mega-climate 3, the main danger to the biosphere would come not from an increasing temperature but from a decreasing (rather than an increasing) CO<sub>2</sub> level which could, in time, fall below 0.5 PAL, causing serious damage to the biosphere. Fortunately, the rates of change due to solar brightening are slow enough that Mega-climate 3 appears to pose no threat to the biosphere for the next 0.5-2 Gyear.
url https://www.ann-geophys.net/13/782/1995/angeo-13-782-1995.pdf
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