Radiative Forcing of Climate Change

@article{Shine2000RadiativeFO,
  title={Radiative Forcing of Climate Change},
  author={Keith P. Shine},
  journal={Space Science Reviews},
  year={2000},
  volume={94},
  pages={363-373}
}
  • K. Shine
  • Published 1 November 2000
  • Environmental Science
  • Space Science Reviews
Our current understanding of mechanisms that are, or may be, acting to cause climate change over the past century is briefly reviewed, with an emphasis on those due to human activity. The paper discusses the general level of confidence in these estimates and areas of remaining uncertainty. The effects of increases in the so-called well-mixed greenhouse gases, and in particular carbon dioxide, appear to be the dominant mechanism. However, there are considerable uncertainties in our estimates of… 

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References

SHOWING 1-10 OF 673 REFERENCES

On Modification of Global Warming by Sulfate Aerosols

Abstract There is increasing evidence that the response of climate to increasing greenhouse gases may be modified by accompanying increases in sulfate aerosols. In this study, the patterns of

The missing climate forcing

Observed climate change is consistent with radiative forcings on several time-scales for which the dominant forcings are known, ranging from the few years after a large volcanic eruption to

Possible change in climate parameters with zero net radiative forcing

There has been much debate over the possibility that radiative cooling due to anthropogenic aerosols may substantially offset global warming from the enhanced greenhouse effect of raised atmospheric

Climate forcings in the industrial era.

Uncertainty in climate forcings have supplanted global climate sensitivity as the predominant issue for long-term climate projections: current trends in GHGClimate forcings are smaller than in popular "business as usual" or 1% per year CO2 growth scenarios.

Global average climate forcing and temperature response since 1750

Estimates are made for the period since 1750 of the major radiative forcing factors thought to be important in climate change. Analysis of these emphasizes the role of biospheric CO2 release and

Climate Forcing by Anthropogenic Aerosols

The aerosol forcing has likely offset global greenhouse warming to a substantial degree, however, differences in geographical and seasonal distributions of these forcings preclude any simple compensation.

Radiative forcing and climate response

We examine the sensitivity of a climate model to a wide range of radiative forcings, including changes of solar irradiance, atmospheric CO2, O3, CFCs, clouds, aerosols, surface albedo, and a “ghost”

Historical evolution of radiative forcing of climate

Simulations of Aerosol Indirect Effect for IPCC Emissions Scenarios

We used a fully coupled climate/chemistry model together with the newly developed IPCC anthropogenic emissions to simulate the climate variation by aerosols. The range of aerosol forcing by the
...