Scientific linkages in global change
Technical Report
·
OSTI ID:5287574
In the atmosphere, certain trace gases both promote global warming and deplete the ozone layer. The primary radiatively active trace gases that affect global warming are carbon dioxide, nitrous oxide, chlorofluorocarbons, methane, and tropospheric ozone. In the troposphere, the atmosphere up to 10 miles above the earth's surface, these compounds function as greenhouse gases. Many of these gases also influence the concentration of ozone in the stratosphere, the atmospheric layer located between 10-30 miles above the earth's surface. The diffuse layer of ozone in the stratosphere protects life on earth from harmful solar radiation. A reduction of the layer could have very important impacts on the earth's systems. Interactions exist in various ecological processes as well. Physical, chemical, and biological activities of plants and animals are affected directly by global climate change and by increased ultraviolet radiation resulting from depletion of stratospheric ozone.
- Research Organization:
- Environmental Protection Agency, Washington, DC (USA). Office of Research and Development
- OSTI ID:
- 5287574
- Report Number(s):
- PB-90-112608/XAB; EPA--600/D-89/126
- Country of Publication:
- United States
- Language:
- English
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Related Subjects
54 ENVIRONMENTAL SCIENCES
540110*
AIR POLLUTION
ATMOSPHERIC CHEMISTRY
CHEMICAL REACTIONS
CHEMISTRY
CLIMATES
DIFFUSION
EARTH ATMOSPHERE
ECOLOGY
ELECTROMAGNETIC RADIATION
GLOBAL ASPECTS
GREENHOUSE EFFECT
LAYERS
OZONE LAYER
PHOTOCHEMICAL REACTIONS
POLLUTION
RADIATIONS
SOLAR RADIATION
STELLAR RADIATION
STRATOSPHERE
TROPOSPHERE
ULTRAVIOLET RADIATION
540110*
AIR POLLUTION
ATMOSPHERIC CHEMISTRY
CHEMICAL REACTIONS
CHEMISTRY
CLIMATES
DIFFUSION
EARTH ATMOSPHERE
ECOLOGY
ELECTROMAGNETIC RADIATION
GLOBAL ASPECTS
GREENHOUSE EFFECT
LAYERS
OZONE LAYER
PHOTOCHEMICAL REACTIONS
POLLUTION
RADIATIONS
SOLAR RADIATION
STELLAR RADIATION
STRATOSPHERE
TROPOSPHERE
ULTRAVIOLET RADIATION