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the Earths radiation budget
the Earths radiation budget

... amount of reflected solar radiation, more radiation will be absorbed by the Earth’s surface, ultimately leading to further warming. Changing the Earth’s albedo to combat climate change Several people have proposed ways to artificially ‘engineer’ the climate to combat man-made climate change by incr ...
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... Our Climate is changing because humans have increased the amount of Greenhouse Gases (GHGs) in the atmosphere. Greenhouse Gases are actually necessary, as they help to keep the earth’s surface warm by trapping the earth’s heat (the greenhouse effect). Without this warmth the earth would be unbearabl ...
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... 23. Which evidence would be least useful for studying past climates? (a) written temperature data (b) tree rings (c) pollen grains (d) ice core samples 24. Which statement was not a finding of the Intergovernmental Panel on Climate Change? (a) Global average surface temperatures increased by about 0 ...
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... that of the moon which has no evidence of life. Only about 1% of the Earth’s atmosphere is made up of naturally occurring greenhouse gases. If this fine balance of gases is increased, there could be significant effects on Earth. These could include increases in the average temperature, changes in th ...
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Introduction - Department of Meteorology and Climate Science

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Climate change

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... Human responsibility for most of the well-documented increase in global average temperatures over the last half century is well established. Further greenhouse gas emissions, particularly of carbon dioxide from the burning of fossil fuels, will almost certainly contribute to additional widespread cl ...
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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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