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This paper is not intended to be a comprehensive discussion of the scientific basis for climate change. Rather, the discussion here is intended to provide a context for the action program we describe. The following is a summary of the findings of the Intergovernmental Panel on Climate Change (IPCC) that shape our program of recommendations.[ii]
The IPCC has concluded that the warming described above is due to human activity. It states:
“Emissions of greenhouse gases and aerosols due to human activities continue to alter the atmosphere in ways that are expected to affect the climate.”[iii]
Among the most striking findings presented :
The IPCC concludes:
“In the light of new evidence and taking into account the remaining uncertainties, most of the observed warming over the last 50 years is likely to have been due to the increase in greenhouse gas concentrations[v].” (Emphasis added)
The IPCC has several scenarios that it uses to project possible stabilization levels for atmospheric CO2. These scenarios, referred to as A1, A2, B1 and B2 use differing assumptions regarding population growth and human environmental impact. They are “business as usual” scenarios that do not take into account GHG emissions mitigation activities. The projected emissions amounts and corresponding atmospheric CO2 concentrations are shown in the charts below (taken from IPCC TAR). These charts show that even under the most optimistic scenario, the atmospheric CO2 stabilizes at a level almost 50% higher than today.
As these charts demonstrate, actions must be taken to stabilize the atmospheric CO2 concentration in order to prevent unprecedented and unknown effects on the climate.
From these projections, IPCC concludes:
“…to maintain a constant future CO2 concentration, anthropogenic CO2 emissions would ultimately have to be reduced to the level of persistent natural sinks.”
This statement is sometimes known as “the scientific (ecological) imperative.” The following chart shows the atmospheric CO2 concentrations that would result under different emissions scenarios. Note that even the most optimistic scenario (B1) results in atmospheric CO2 that is stabilized at a level (475 ppm-575 ppm); far higher than today.
Figure 2 shows how emissions would have to decrease in order for the atmospheric CO2 concentration to stabilize at various levels. Note that the lowest stabilization level (450 ppm) is only attainable if annual emissions of CO2 start to decline within the 30-40 years.
Finally, Figure 3 shows the range of temperature increase that is projected to result under the various emission scenarios. The most optimistic scenario (B1) is predicted to result in an increase of between one degree and three degrees Celsius by the year 2100. The least optimistic scenario (A1F1) is predicted to result in a three degree to six degree Celsius increase by the year 2100.
More recent experiments with more accurate models show that an even larger increase in temperature can be expected for a given concentration.