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The changing nature of flooding across the central United States
The changing nature of flooding across the central United States

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urbanization and climate change in small island developing states

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Working Paper 165 - Dechezlepretre et al 2015 (opens in new window)
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... However, one could further questions (P2) by claiming that instead of the atmosphere the totality of all global commons is owned by everyone equally (cf. Caney, 2012: 268-271). Assuming for the sake of argument that this claim is correct, it would result in a very complex allocation procedure. The r ...
NBER WORKING PAPER SERIES INCORPORATING CLIMATE UNCERTAINTY INTO ESTIMATES OF CLIMATE
NBER WORKING PAPER SERIES INCORPORATING CLIMATE UNCERTAINTY INTO ESTIMATES OF CLIMATE

... adaptation beyond what is implied in the historical relationships. While such adaptation could dampen projected impacts, predicting and quantifying the degree of adaptation to changing climate during 2080-2100 is inherently speculative, and as discussed below, there is surprisingly little evidence o ...
PDF
PDF

... little, too fast”; developing countries should play a more substantial role and receive incentives to participate; implementation should focus on market-based approaches, especially those with price mechanisms; and participation and compliance incentives are inadequately addressed by most proposals. ...
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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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