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Climate change justice and the global policy mix
Climate change justice and the global policy mix

... Recent research indicates that achieving a 29-70 per cent chance of avoiding dangerous climate change by meeting the 2oC objective would require policies being adopted that result in no more than 2000 billion tonnes of carbon dioxide (CO2)-equivalent being emitted in the 2000-2050 period, of which r ...
Thermal Expansion Activity (Teacher version)
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... Global Mean Sea Level (GMSL) has risen by 4 to 8 inches (10 to 20 centimeters). However, the annual rate of rise over the past 20 years has been 0.13 inches (3.2 millimeters) a year, roughly twice the average speed of the preceding 80 years. Over the past century, the burning of fossil fuels and oth ...
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... The Law on protection and rescue prescribes a set of measures and activities to prevent danger of natural disasters, technological accidents and other disasters. In order to effectively protect the population and the material heritage against possible disasters and preventing the spreading of risk, ...
LEARN ABOUT… Climate change and ozone depletion
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SUBSTITUTION OF NATURAL GAS FOR COAL: CLIMATIC
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... higher carbon contents, is one of the principal methods suggested to reduce carbon dioxide emissions from energy consumption in the near future (e.g., E7, 2000; Nakicenovic, 2000; Audus, 1999; ORNL, 1997; Watson et al., 1996). In this study, we use the replacement of coal use by natural gas in the e ...
Paying for carbon emissions reduction
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Volume 3: Climate and Global Change and Risks
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THINKING LONG TERM - World Resources Institute
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wetlands, biodiversity and climate change
wetlands, biodiversity and climate change

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there once was an island te henua e nnoho
there once was an island te henua e nnoho

... 5. In Chapter 3, we travel to the garden island with Teloo Fakatutufenua where he shows us his garden, from which he harvests giant swamp taro. The giant swamp taro is intolerant of the saltwater. In areas where it once grew, there is now none. Teloo sadly says, “There is nothing we can do ...
The Myopia of Imperfect Climate Models: The Case of UKCP09
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House science testimony apr 15 final - Climate Etc.
House science testimony apr 15 final - Climate Etc.

... Human-caused warming depends not only on increases in greenhouse gases but also on how ‘sensitive’ the climate is to these increases. Climate sensitivity is defined as the global surface warming that occurs when the concentration of carbon dioxide in the atmosphere doubles. If climate sensitivity is ...
East Africa
East Africa

... applied in our work, including statistical tests, are discussed in Part I. Return levels are estimated from the fitted GPD. Return levels are frequently used in extreme precipitation studies in climate research (e.g., Kharin and Zwiers 2000; Meehl et al. 2005; Kharin et al. 2007) because of the simp ...
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The Effects and Linkages of Deforestation and Temperature on

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Growing trees to sequester carbon in the UK
Growing trees to sequester carbon in the UK

... levels, and in many areas by enhanced atmospheric N deposition. In the UK, this CO2 and Nfertilization sink could be of the order 2 MtC a–1. All these terrestrial sinks are offset by losses of soil organic carbon in other UK land areas due to increased cultivation, urbanization, drainage of peatland ...
Environment, Politics and Development Working Paper Series
Environment, Politics and Development Working Paper Series

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Operating in Limits: Defining an Australian
Operating in Limits: Defining an Australian

... way to link short- and long-term emissions reduction targets to a scientifically robust ‘carbon budget’ for the nation. The development of this national carbon budget is now central to the deliberations of the Climate Change Authority (the Authority). The Authority is an independent body, which prov ...
Climate change: a framework for a global agreement in 2015
Climate change: a framework for a global agreement in 2015

... responsible for developing, passing and amending laws and ensuring that these are implemented, as well as approving national budgets and holding climate negotiators accountable. It is crucial to build capacity amongst legislators in order to maximise their potential to have a positive influence on i ...
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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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