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New estimates of radiative forcing due to well mixed greenhouse gases

Geophysical Research Letters · 1998 · Vol. 25(14) · pp. 2715–2718
Gunnar MyhreE. J. HighwoodKeith P. ShineFrøde Stordal

Abstract

We have performed new calculations of the radiative forcing due to changes in the concentrations of the most important well mixed greenhouse gases (WMGG) since pre‐industrial time. Three radiative transfer models are used. The radiative forcing due to CO 2 , including shortwave absorption, is 15% lower than the previous IPCC estimate. The radiative forcing due to all the WMGG is calculated to 2.25 Wm −2 , which we estimate to be accurate to within about 5%. The importance of the CFCs is increased by about 20% relative to the total effect of all WMGG compared to previous estimates. We present updates to simple forcing‐concentration relationships previously used by IPCC.

Atmospheric and Environmental Gas DynamicsAtmospheric chemistry and aerosolsAtmospheric Ozone and ClimateRadiative forcingForcing (mathematics)Greenhouse gasRadiative transferShortwaveEnvironmental scienceAtmospheric sciencesGreenhouse effectAtmospheric radiative transfer codesClimatology
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References
Radiative forcing and climate response
Journal of Geophysical Research Atmospheres · 1997 · 2,398 citations
Climate change—The IPCC scientific assessment
Environment International · 1991 · 1,309 citations
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