Mount Pinatubo aerosols, chlorofluorocarbons, and ozone depletion

Journal Article · Fri Aug 28 04:00:00 EDT 1992 · Science (Washington, D.C.); (United States)

DOI:https://doi.org/10.1126/science.257.5074.1239· OSTI ID:7271257

Brasseur, G; Granier, C ^[1]

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1. National Center for Atmospheric Research, Boulder, CO (United States)

The injection into the stratosphere of large quantities of sulfur during the June 1991 eruption of Mount Pinatube (Philippines) and the subsequent formation of sulfate aerosol particles have generated a number of perturbations in the atmosphere with potential effects on the Earth's climate. Changes in the solar and infrared radiation budget caused by the eruption should produce a cooling of the troposphere and a warming of the lower stratosphere. These changes could affect atmospheric circulation. In addition, heterogeneous chemical reactions on the surface of sulfate aerosol particles render the ozone molecules more vulnerable to atmospheric chlorine and hence to man-made chlorofluorocarbons.

• OSTI ID: 7271257
• Journal Information: Science (Washington, D.C.); (United States), Journal Name: Science (Washington, D.C.); (United States) Vol. 257:5074; ISSN SCIEA; ISSN 0036-8075
• Country of Publication: United States
• Language: English

Related Subjects

29 ENERGY PLANNING, POLICY, AND ECONOMY
290301 -- Energy Planning & Policy-- Environment
Health
& Safety-- Regional & Global Environmental Aspects-- (1992-)
54 ENVIRONMENTAL SCIENCES
540120* -- Environment
Atmospheric-- Chemicals Monitoring & Transport-- (1990-)
AEROSOLS
ASIA
CHLOROFLUOROCARBONS
CLIMATIC CHANGE
COLLOIDS
DEVELOPING COUNTRIES
DISPERSIONS
EARTH ATMOSPHERE
ENVIRONMENTAL EFFECTS
ERUPTION
ISLANDS
LAYERS
ORGANIC CHLORINE COMPOUNDS
ORGANIC COMPOUNDS
ORGANIC FLUORINE COMPOUNDS
ORGANIC HALOGEN COMPOUNDS
OXYGEN COMPOUNDS
OZONE LAYER
PHILIPPINES
RADIATIONS
SOLAR RADIATION
SOLS
STELLAR RADIATION
STRATOSPHERE
SULFATES
SULFUR COMPOUNDS
TROPOSPHERE
VOLCANOES