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Quantifying Mineral Dust Mass Budgets:Terminology
Quantifying Mineral Dust Mass Budgets:Terminology

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Chapter 8: Cross-cutting issues
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Chapter 3 – The cost-effective path to 2050
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Global Sources and Pathways of Mercury in the Context of Human

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High-impact Sectors: the Challenge of Reporting on Climate Change
High-impact Sectors: the Challenge of Reporting on Climate Change

... air and ocean temperatures, widespread melting of snow and ice and rising global average sea level. (p. 2) most of the observed increase in global average temperatures since the mid-20th century is very likely due to the observed increase in anthropogenic GHG concentrations. It is likely that there ...
Crop response to elevated CO2 and world food supply A
Crop response to elevated CO2 and world food supply A

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CDP Climate Change 2015 - Coca
CDP Climate Change 2015 - Coca

... embedded into our business-planning activities. Climate change presents a significant long-term risk. This includes the risk of rising energy costs, threats to our agricultural supply chain, availability of water to our production facilities and suppliers, carbon taxes. Adverse weather conditions co ...
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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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