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Titlebook: Image: An Integrated Model to Assess the Greenhouse Effect; Jan Rotmans Book 1990 Kluwer Academic Publishers 1990 agriculture.biosphere.ca

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The Methane Module,n et al., 1985, Wang and Molnar, 1985). Analysis of air contained in ice cores indicates that the methane concentration has been ca. 0.7 . for maybe thousands of years (Khalil and Rasmussen, 1982, and 1987). Around 1700 A.D. the concentration seems to have started increasing slowly to ca. 0.9 . arou
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The N2O Module,in soil and water and is removed from the atmosphere much more slowly than methane. The yearly growth in the N.O emission trend varied from 0.1% at the beginning of this century to 1.3% in the last 10 years. The current average concentration of N.O is about 0.308 . and is increasing at about 0.2 to
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The Climate Module,rstanding of this climate system is still not satisfactory. Climate models try to consider the primary processes, radiation, dynamics and surface processes, and their interactions within the climate system (Shine and Henderson-Sellers, 1983, Dickinson, 1986). Climate modelling has developed rapidly
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Temperature Increasing Potential,eenhouse gas emissions. Here the concept of Temperature Increasing Potential (TIP) is introduced as a greenhouse counterpart to the ozone depleting potential (ODP). To obtain the relationship between an emission and its associated effect on temperature both the model approach (IMAGE) and the analyti
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Sensitivity Analysis,ieze, 1990, Rotmans et al., 1990), is used to perform sensitivity experiments with IMAGE. In this chapter it is explained how the technique of metamodelling enables us to search for a relationship between input and output variables of IMAGE and how experimental designs can be used to carry out exper
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