Los aerosoles, la microfísica de las nubes y la nubosidad fraccionada.

Science (New York, N.Y.)
|September 15, 1989
PubMed
Resumen

El aumento de las concentraciones de aerosoles sobre los océanos puede aumentar la nubosidad de bajo nivel al reducir la llovizna. Esto aumenta el albedo global, contribuyendo al efecto de enfriamiento de la superficie de la Tierra.

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