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Climate change and impacts in the Eastern Mediterranean and the
Climate change and impacts in the Eastern Mediterranean and the

... occasional droughts, and mild, relatively wet winters (Bolle 2003; Lionello et al. 2006). In the southern EMME, an arid hot desert climate prevails, where precipitation is low and vegetation scanty (Issar and Zohar 2007). The temperature and precipitation gradients across the region are remarkable. ...
Impacts of Climate Change
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... Climate as a Dynamic, Chaotic System It is important for those interested in the human significance of climate change to consider the fallacy of averages. While the SRES A2 scenario suggests that the average temperature of Earth will warm by between 0.7 and 2.0° Celsius (with an average of about 1. ...
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A Summary of Climate Change Risks for South East

... Climate change will pose a number of risks to health and healthcare provision in the South East: • The CCRA notes that increased flooding may lead to increased number of deaths, injuries, and people suffering from mental health effects due to loss of homes and property and dislocation. • Impacts s ...
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Assessing climate change and climate variability impacts in Burkina

... for seasonal forecasting, (ii) complex topography (associated with the Guinean Highlands, Jos Plateau in Nigeria and Cameroon mountains. Predictions of climate change (and natural variability) are dependent on General Circulation Models (GCMs). Predictions from GCMs of climate change in West Africa ...
Presentation (power point file)
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The Influence on Climate Change of Differing Scenarios for Future

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Working Paper WP 2015-06 April 2015
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RobockEthicsOslo - Alan Robock

... implement geoengineering, and if so how much? Whose hand would be on the planetary thermostat? The principle of informed consent governs medical interventions. How could we get the informed consent of the entire planet? If geoengineering were ever implemented, every climate extreme would be blamed o ...
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... one of 27 chapters of what is generally seen as an authoritative report, the Stern Review had a powerful effect on governments. It forcefully made the argument that, globally, policies to reduce greenhouse gas emissions will be in the interest of economic growth rather than hampering it: though it r ...
Climate Change and Its Causes - The Science and Public Policy
Climate Change and Its Causes - The Science and Public Policy

... The IPCC acknowledges that if the atmospheric concentration of CO2 doubles the global average temperature could rise between 1.5 and 4.5 oC at equilibrium. The variability of climate sensitivity to CO2 is shown in Figure 4, which demonstrates an even wider sensitivity temperature range [5]. If green ...
Sustainable Claims Management
Sustainable Claims Management

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1 introduction to atmosphere and climate
1 introduction to atmosphere and climate

... particles, and small amounts of other gases, such as carbon dioxide, nitrous oxide and methane (0.1%) (Twomey, 1977). These gases can either be free in the air or associated with water vapour. Of the trace gases present in the atmosphere, water vapour is the most important greenhouse gas as it allow ...
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... that the number of intense extratropical cyclones may increase under climate change (whereas the total number of storms might be reduced), citing a set of research works reaching this conclusion (e.g., Lambert and Fyfe, 2005). Third, the Fourth Assessment Report describes that the “consistent” resul ...
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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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