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Aerosols, Climate, and the Hydrological Cycle

Bibliographic Data

ID23322589
AuthorsV Ramanathan (0000-0002-3534-5987, Scripps Institution of Oceanography, University of California at San Diego, CA 92093, USA., corresponding author), Paul J Crutzen (Scripps Institution of Oceanography), J T Kiehl (0000-0001-5812-6552, NSF National Center for Atmospheric Research), Daniel Rosenfeld (0000-0002-0784-7656, Hebrew University of Jerusalem)
Year2001
Volume294
Issue5549
Pages2119-2124
Publication date2001-12-07
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueScience (JOURNAL)
Journal identifiersISSN: 0036-8075 • E-ISSN: 0193-4511
PublisherAmerican Association for the Advancement of Science (AAAS) (PUBLISHER)
DOI10.1126/science.1064034
PMID11739947
OpenAlexW2119744638
LanguageEN
Citations received66
References cited43

Human activities are releasing tiny particles (aerosols) into the atmosphere. These human-made aerosols enhance scattering and absorption of solar radiation. They also produce brighter clouds that are less efficient at releasing precipitation. These in turn lead to large reductions in the amount of solar irradiance reaching Earth's surface, a corresponding increase in solar heating of the atmosphere, changes in the atmospheric temperature structure, suppression of rainfall, and less efficient removal of pollutants. These aerosol effects can lead to a weaker hydrological cycle, which connects directly to availability and quality of fresh water, a major environmental issue of the 21st century.

Aerosol · Atmosphere (unit) · Atmospheric sciences · Geography · Irradiance · Lead (geology) · Meteorology · Physics · Precipitation · Solar irradiance · Water cycle · Atmospheric aerosols and clouds · Atmospheric chemistry and aerosols · Ecology · Environmental Science · Geology · Solar Radiation and Photovoltaics

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Unique citing works66
Citations per year2,75
Citation span2002 - 2026 (25)
Citation velocitycurrent
Highly citedNo
Citation typesNeutral: 62
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