Climate Modification by Atmospheric Aerosols
- 9 June 1967
- journal article
- research article
- Published by American Association for the Advancement of Science (AAAS) in Science
- Vol. 156 (3780) , 1358-1359
- https://doi.org/10.1126/science.156.3780.1358
Abstract
Theoretical considerations and empirical evidence indicate that atmospheric turbidity, a function of aerosol loading, is an important factor in the heat balance of the earth-atmosphere system. Turbidity increase over the past few decades may be primarily responsible for the decrease in worldwide air temperatures since the 1940's.This publication has 8 references indexed in Scilit:
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