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Greenhouse Gases Global Warming Potential
Greenhouse Gases: Global Warming Potential
Table data referenced to the Updated Decay Response for the Bern Carbon Cycle Model and Future CO2 Atmospheric Concentrations Held Constant at Current Levels
a Water vapor has been omitted because of its shorter average residence time in the atmosphere (i.e., about 7 days).
b Derived from the Bern carbon cycle model.
cThe global warming potential (GWP) for methane includes indirect effects of tropospheric ozone production and stratospheric water vapor production.
d The GWPs for ozone-depleting substances (including all CFCs, HCFCs, and halons, whose direct GWPs have been given in previous reports) are a sum of a direct (positive) component and an indirect (negative) component which depends strongly upon the effectiveness of each substance for ozone destruction. Generally, the halons are likely to have negative net GWPs, while those of the CFCs are likely to be positive over both 20-and 100- year time horizons.
Houghton, John T., L. G. Meiro Filho, B.A. Callander, N. Harris, A. Kattenburg, and K. Maskell, Climate Change 1995: The Science of Climate Change, Cambridge University Press, June 1996.
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