chapter - Atmospheric and Oceanic Science
chapter - Atmospheric and Oceanic Science
chapter - Atmospheric and Oceanic Science
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Global climatic change<br />
On the base of these <strong>and</strong> other facts, the Inter-governmental Panel for the<br />
Climatic Change (IPCC 2001a) in its report of the year 2001 has concluded that the<br />
trend to warming observed in the twentieth century has an important component of<br />
human origin.<br />
9.7. The climate in the twenty first century<br />
The evolution of the emission of GHG in the future will depend on numerous<br />
factors whose prediction is quite complex. They are the economic <strong>and</strong> demographic<br />
growth, the technological changes <strong>and</strong> even the development towards a society<br />
with more or less equity. Finally, but not less important, it will depend of the collective<br />
answers of the humanity to reduce or at least to diminish the rate of growth<br />
of the emission.<br />
Since all these factors are very difficult to foresee, the only possibility is to<br />
build possible socioeconomic scenarios of the future. The building <strong>and</strong> characteristics<br />
of these scenarios are discussed in <strong>chapter</strong> 13. The different scenarios suppose<br />
dissimilar levels of economic activity that imply in turn different emissions scenarios.<br />
It is possible to build as many emission scenarios as arise from the combinations<br />
of the driven factors of the level of economic activity <strong>and</strong> of its characteristics,<br />
without certainty on which will be the one really happening. However, for a<br />
given scenario of GHG emissions throughout time, it will be a corresponding scenario<br />
of concentration evolution of these gases.<br />
The effect of GHG concentrations in the climate is studied with the help of<br />
global climate models (GCM) that simulate the climatic system in almost all its<br />
complexity. These models represent the physical processes of the sea, the atmosphere,<br />
the soil <strong>and</strong> the cryosphere, <strong>and</strong> simulate its evolution using huge computers.<br />
In <strong>chapter</strong> 11, they are described in more detail. Only the most sophisticated<br />
GCM have been capable of reproducing, forced by the observed evolution of GHG<br />
concentrations, the global climate global changes observed during the industrial<br />
period. This generates certain confidence in their capacity to simulate the global<br />
changes of the future climate.<br />
The different GCM project different values of the global temperature, still<br />
under the same socio-economic scenarios. Nevertheless, they all give the same<br />
qualitative response, important warming throughout the twenty first century for any<br />
of the socioeconomic scenarios.<br />
The GCM are a reliable methodology to assess climate changes at global<br />
scale, but they still have a limited capacity to simulate the climate at regional scale,<br />
underst<strong>and</strong>ing for such the one that goes from a locality up to a continent. Although<br />
the different models are consistent among one another in terms of their predictions<br />
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