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“climate change” or “global warming” will find it useful.
“climate change” or “global warming” will find it useful.

... rain down on Tokyo. Why the sudden onslaught of deadly weather? Global warming has triggered a series of natural disasters—including a monster storm that’s racing south from the Arctic. And when the behemoth hits in 96 hours, beware: It will turn New York City into a frozen wasteland. Panicked? Don’ ...
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Climate Change Country Profile

... As Italy's Alpine glaciers recede, the melted water contributes to rising sea levels. The loss of glaciers also What remains of the Calderone glacier in Abruzzo. Photo: Guidosky increases global temperatures as the large tracts of white ice are no longer present to reflect the sun's rays back out to ...
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... Rainforests play an important part in the climate system. Perhaps the most significant role of the rainforest in climate is its role as a carbon dioxide sink. While they only cover about 6% of the Earth’s land surface, almost 30% of global soil carbon stocks are contained in their soils (“H. Rainfor ...
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NGSS Earth Science Weather and Climate Unit

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Parry

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AOSS_NRE_480_L15_International_Policy_20150226

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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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