DOI: 10.1126/science.245.4923.1227. Aerosols, Cloud Microphysics, and Fractional Cloudiness

Aerosols, Cloud Microphysics, and Fractional Cloudiness

10.1126/science.245.4923.1227

Crossref journal-article

American Association for the Advancement of Science (AAAS)

Science (221)

Abstract

Increases in aerosol concentrations over the oceans may increase the amount of low-level cloudiness through a reduction in drizzle—a process that regulates the liquid-water content and the energetics of shallow marine clouds. The resulting increase in the global albedo would be in addition to the increase due to enhancement in reflectivity associated with a decrease in droplet size and would contribute to a cooling of the earth's surface.

Bibliography

Albrecht, B. A. (1989). Aerosols, Cloud Microphysics, and Fractional Cloudiness. Science, 245(4923), 1227â1230.

Authors 1

Bruce A. Albrecht (first)

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Dates

Type	When
Created	18 years, 10 months ago (Oct. 5, 2006, 5:21 p.m.)
Deposited	1 year, 7 months ago (Jan. 12, 2024, 11:48 a.m.)
Indexed	10 minutes ago (Aug. 29, 2025, 1:28 a.m.)
Issued	35 years, 11 months ago (Sept. 15, 1989)
Published	35 years, 11 months ago (Sept. 15, 1989)
Published Print	35 years, 11 months ago (Sept. 15, 1989)

Funders 0

None

BibTeX

@article{Albrecht_1989, title={Aerosols, Cloud Microphysics, and Fractional Cloudiness}, volume={245}, ISSN={1095-9203}, url={http://dx.doi.org/10.1126/science.245.4923.1227}, DOI={10.1126/science.245.4923.1227}, number={4923}, journal={Science}, publisher={American Association for the Advancement of Science (AAAS)}, author={Albrecht, Bruce A.}, year={1989}, month=sep, pages={1227–1230} }

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