Climate Modification by Atmospheric Aerosols
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...
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Veröffentlicht in: | Science (American Association for the Advancement of Science) 1967-06, Vol.156 (3780), p.1358-1359 |
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Hauptverfasser: | , |
Format: | Artikel |
Sprache: | eng |
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Online-Zugang: | Volltext |
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Zusammenfassung: | 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. |
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ISSN: | 0036-8075 1095-9203 |
DOI: | 10.1126/science.156.3780.1358 |