TheGlobalWarmingInfo.com

 

 

 

 

 

 

 

 

 

GLOBAL WARMING

CLIMATE MODELS

Scientists have studied global warming with computer models of the climate. These models predict that the net effect of adding greenhouse gases will be a warmer climate in the future. However, even when the same assumptions of fossil fuel consumption and CO2 emission are used, the amount of predicted warming varies between models and there still remains a considerable range of climate sensitivity.

Including model and future greenhouse gas uncertainty, the IPCC anticipates a warming of 1.1 °C to 6.4 °C (2.0 °F to 11.5 °F) between 1990 and 2100. They have also been used to help investigate the causes of recent climate change by comparing the observed changes to those that the models predict from various natural and human derived forcing factors.

Climate models can produce a good match to observations of global temperature changes over the last century . These models do not unambiguously attribute the warming that occurred from approximately 1910 to 1945 to either natural variation or human effects; however, they suggest that the warming since 1975 is dominated by man-made greenhouse gas emissions.

Most global climate models, when run to predict future climate, are forced by imposed greenhouse gas scenarios, generally one from the IPCC Special Report on Emissions Scenarios (SRES). Less commonly, models may be run by adding a simulation of the carbon cycle; this generally shows a positive feedback, though this response is uncertain (under the A2 SRES scenario, responses vary between an extra 20 and 200 ppm of CO2). Some observational studies also show a positive feedback.

The representation of clouds is one of the main sources of uncertainty in present-generation models, though progress is being made on this problem. There is also an ongoing discussion as to whether climate models are neglecting important indirect and feedback effects of solar variability.

 

INDEX

 

 

   Terminology
   History of warming
   Causes
 Greenhouse gases in the atmosphere
 Solar variation

   Attributed and expected effects
   Mitigation

 Kyoto Protocol
   Climate models
   Other related issues

 Ocean acidification
 Relationship to ozone depletion
 Relationship to global dimming
 Pre-human global warming
 Pre-industrial global warming
               References

 

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