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Climate Impact of Increasing Atmospheric Carbon Dioxide

Science28 Aug 1981Vol 213, Issue 4511pp. 957-966DOI: 10.1126/science.213.4511.957

Abstract

The global temperature rose by 0.2°C between the middle 1960's and 1980, yielding a warming of 0.4°C in the past century. This temperature increase is consistent with the calculated greenhouse effect due to measured increases of atmospheric carbon dioxide. Variations of volcanic aerosols and possibly solar luminosity appear to be primary causes of observed fluctuations about the mean trend of increasing temperature. It is shown that the anthropogenic carbon dioxide warming should emerge from the noise level of natural climate variability by the end of the century, and there is a high probability of warming in the 1980's. Potential effects on climate in the 21st century include the creation of drought-prone regions in North America and central Asia as part of a shifting of climatic zones, erosion of the West Antarctic ice sheet with a consequent worldwide rise in sea level, and opening of the fabled Northwest Passage.

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Science
Volume 213 | Issue 4511
28 August 1981

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Published in print: 28 August 1981

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J. Hansen
Atmospheric physicists at the NASA Institute for Space Studies, Goddard Space Flight Center, New York 10025
D. Johnson
Atmospheric physicists at the NASA Institute for Space Studies, Goddard Space Flight Center, New York 10025
A. Lacis
Atmospheric physicists at the NASA Institute for Space Studies, Goddard Space Flight Center, New York 10025
S. Lebedeff
Atmospheric physicists at the NASA Institute for Space Studies, Goddard Space Flight Center, New York 10025
P. Lee
Atmospheric physicists at the NASA Institute for Space Studies, Goddard Space Flight Center, New York 10025
D. Rind
Atmospheric physicists at the NASA Institute for Space Studies, Goddard Space Flight Center, New York 10025
G. Russell
Atmospheric physicists at the NASA Institute for Space Studies, Goddard Space Flight Center, New York 10025

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