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Lands` End to the Arctic
Lands` End to the Arctic

... The final chapters ask what lessons Greenland has taught us. The documentation of abrupt climate change gleaned from its ice offers a sober warning of the consequences of a rapidly warming Arctic, including the summertime loss of Arctic sea ice, the accelerating thawing of the permafrost surrounding ...
Exploring Climate Change
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... temperatures. The reality is somewhere in between and is much more complex than either extreme would like it to be. The scientific consensus is that warming of ocean surface waters is likely to lead to an increase in the intensity of tropical storms, with higher peak wind speeds and heavier rainfall ...
PPT - unece
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... Surface: Air temperature, Precipitation, Air pressure Upper-air: Radiation, Upper-air temperature, Water vapour, Cloud properties, etc. Composition: Carbon dioxide, Methane, Ozone, etc. ...
L18.ppt
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... Effect of greenhouse gases: H2O, CO2, CH4, . . . • the sun’s visible light can penetrate through the atmosphere to the earth’s surface and heat it • the visible light energy is converted to thermal light energy • the thermal radiation is reflected from the greenhouse gases in the atmosphere • CO2 c ...
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... 2007: Supreme Court ruled that Clean Air Act covered greenhouse gases. 2009: Obama proposed strong cuts, House passed strong bill, but it died. 2009: EPA: “The Administrator is proposing to find that the current and projected concentrations of the mix of six key greenhouse gases— carbon dioxide (CO2 ...
WhySciTeachersWEB ppt
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Climate Change – Can science teachers play a part
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... Since 2005, the Academies of Science for the G8+5 countries have called on world leaders to limit the threat of climate change. We have advised prompt action to deal with the causes of climate change and cautioned that some climate impacts are inevitable. However, progress in reducing global greenh ...
Climate Fact Sheet - South Carolina Sea Grant Consortium
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... of species and biodiversity. While governments and non-governmental organisations have worked hard to control it, there has never been a real motivation, or urgency to act until now. Tackling the problem is complex and needs a coordinated global effort. So what’s new now? Well the eyes of the world ...
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www.stanford.edu/group/MERGE/GERAD1.pdf
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... as a benefit-cost problem – reaching agreement on an international control system that leads to the temperature limit which minimizes the discounted present value of abatement costs and damages. This is a more ambitious goal. It requires us to define the disutility that is associated with varying am ...
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Global Climate Change: Intellectual Response of Civil
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Modelling regional responses by marine pelagic ecosystems to
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... greater ability to withstand changes in temperature. But, there is no doubt that marine life is being affected at this time. It may be more due to pollution and to ozone hole effects than to global warming. NCSS- RHinelander, WI, BEn: Do wildfires smoke have any part in global warming? Go North! Spe ...
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... One per cent of the atmosphere is made up of greenhouse gases. These are water vapour, carbon dioxide (CO2), methane (CH4), nitrous oxide (N2O). So what’s the fuss about? It’s really more than a fuss. The natural balance of greenhouse gases has been ruined in the last two hundred years. Things that ...
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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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