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
Hauptverfasser: McCormick, Robert A., Ludwig, John H.
Format: Artikel
Sprache:eng
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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.
ISSN:0036-8075
1095-9203
DOI:10.1126/science.156.3780.1358