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Using Marginal Abatement Cost Curves (MACC) to realize the economic appraisal of Climate Smart Agriculture policy options
Using Marginal Abatement Cost Curves (MACC) to realize the economic appraisal of Climate Smart Agriculture policy options

... The AFOLU sector (Agriculture, Forestry, Land Use) is directly linked with climate change issues, on an environmental aspect as well as on an economical and social aspect (food security). On the one hand, the sector directly contributes to climate change. Indeed, agriculture represents 14% of the to ...
Uganda National Adaptation Programmes of Action
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Text (Open Access) - Reading`s CentAUR

... T47L71 chemistry-climate model was run in a configuration with specified SSTs, sea ice, and greenhouse gases (GHGs). It includes standard stratospheric chemistry accounting for Cly -Bry -Ox -HOx -NOx catalytic cycles and polar stratospheric cloud (PSC) chemistry on stratospheric ternary solution (STS) ...
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The Global Climate Observing System Programme The Global

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climate change and water quality in the great lakes region
climate change and water quality in the great lakes region

... Biological productivity is expected to increase with moderate temperature increases. Zoogeographical boundaries move in a changing climate. Introduction of invasive species could be exacerbated. Existing community structures and interactions may change. A changing climate is expected to lead to redu ...
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Climate change feedback



Climate change feedback is important in the understanding of global warming because feedback processes may amplify or diminish the effect of each climate forcing, and so play an important part in determining the climate sensitivity and future climate state. Feedback in general is the process in which changing one quantity changes a second quantity, and the change in the second quantity in turn changes the first. Positive feedback amplifies the change in the first quantity while negative feedback reduces it.The term ""forcing"" means a change which may ""push"" the climate system in the direction of warming or cooling. An example of a climate forcing is increased atmospheric concentrations of greenhouse gases. By definition, forcings are external to the climate system while feedbacks are internal; in essence, feedbacks represent the internal processes of the system. Some feedbacks may act in relative isolation to the rest of the climate system; others may be tightly coupled; hence it may be difficult to tell just how much a particular process contributes. Forcings, feedbacks and the dynamics of the climate system determine how much and how fast the climate changes. The main positive feedback in global warming is the tendency of warming to increase the amount of water vapor in the atmosphere, which in turn leads to further warming. The main negative feedback comes from the Stefan–Boltzmann law, the amount of heat radiated from the Earth into space changes with the fourth power of the temperature of Earth's surface and atmosphere.Some observed and potential effects of global warming are positive feedbacks, which contribute directly to further global warming. The Intergovernmental Panel on Climate Change's (IPCC) Fourth Assessment Report states that ""Anthropogenic warming could lead to some effects that are abrupt or irreversible, depending upon the rate and magnitude of the climate change.""
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